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class="user-summary-container"><div class="social-profile-avatar-container"><img class="profile-avatar u-positionAbsolute" alt="Victor Medina" border="0" onerror="if (this.src != '//a.academia-assets.com/images/s200_no_pic.png') this.src = '//a.academia-assets.com/images/s200_no_pic.png';" width="200" height="200" src="https://0.academia-photos.com/30199075/9444125/13411765/s200_victor.medina.jpg" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Victor Medina</h1><div class="affiliations-container fake-truncate js-profile-affiliations"></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Victor" data-follow-user-id="30199075" data-follow-user-source="profile_button" data-has-google="false"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">add</span>Follow</button><button class="ds2-5-button hidden profile-cta-button grow js-profile-unfollow-button" data-broccoli-component="user-info.unfollow-button" data-click-track="profile-user-info-unfollow-button" data-unfollow-user-id="30199075"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">done</span>Following</button></div></div><div class="user-stats-container"><a><div class="stat-container js-profile-followers"><p class="label">Followers</p><p class="data">340</p></div></a><a><div class="stat-container js-profile-followees" data-broccoli-component="user-info.followees-count" data-click-track="profile-expand-user-info-following"><p class="label">Following</p><p class="data">40</p></div></a><a><div class="stat-container js-profile-coauthors" data-broccoli-component="user-info.coauthors-count" data-click-track="profile-expand-user-info-coauthors"><p class="label">Co-author</p><p class="data">1</p></div></a><span><div class="stat-container"><p class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="user-bio-container"><div class="profile-bio fake-truncate js-profile-about" style="margin: 0px;">I have experience in geologic area: cateo, prospection, and maping. I am an assistant in geology in the company compumet eirl, I also know about administrative procedures in SSO (Occupational Safety and Health). My roles in field work as project assistant was sampling and cabinet work using the GIS platforms (AutoCAD, CivilCAD, ArcGIS).<br /><br />https://vmedina.geoxnet.com/<br /><span class="u-fw700">Phone: </span>930268127<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="30199075" href="https://www.academia.edu/Documents/in/Engineering_Geology"><div id="js-react-on-rails-context" style="display:none" 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data-dom-id="Pill-react-component-e3678166-26ed-4b41-9982-83eda9f552e1"></div> <div id="Pill-react-component-e3678166-26ed-4b41-9982-83eda9f552e1"></div> </a></div></div><div class="external-links-container"><ul class="profile-links new-profile js-UserInfo-social"><li class="profile-profiles js-social-profiles-container"><i class="fa fa-spin fa-spinner"></i></li></ul></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Victor Medina</h3></div><div class="js-work-strip profile--work_container" data-work-id="29741804"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/29741804/PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN"><img alt="Research paper thumbnail of PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN" class="work-thumbnail" src="https://attachments.academia-assets.com/50198758/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/29741804/PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN: IMPLICATIONS FOR HYDROCARBON OCCURRENCE AT THE...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN: IMPLICATIONS FOR HYDROCARBON OCCURRENCE AT THE SOUTH LIBERTY SALT DOME<br /><br />Generación de Petróleo en la Cuenca Sureste de Texas:<br />Implicaciones para la ocurrencia de Hidrocarburos<br /> en el Domo Salino “South Liberty”<br /><br />Las Características Geoquímicas de Hidrocarburos del yacimiento “South Liberty”, condado Liberty-Texas, fueron integradas a la estratigrafía local, presión, temperatura, datos sísmicos y la química del agua para determinar su origen, madurez y vías de migración de hidrocarburos asociados con el Domo de Sal en el Sur-este de ”Texas Gulf Coast”.  Catorce muestras de aceite crudo fueron obtenidas de los reservorios de ligera-geopresurización "Cook Mountain" y "Yegua" (ambos del Eoceno) y "Frio" (Oligoceno) (189-2886 metros [3245-9469 pies]) fueron analizados mediante Cromatografía de Gases (GC) y Espectrometría de masas GC-mass.  Los datos de presión y temperatura de los 36 pozos fueron usados para modelar la historia de la maduración termal en las proximidades del domo.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2749c475adc602b07ea44aaa53c7bb79" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50198758,"asset_id":29741804,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50198758/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="26270402"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/26270402/Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral"><img alt="Research paper thumbnail of Secuencias Sedimentarias del Rio Huaura - Sector Huaral" class="work-thumbnail" src="https://attachments.academia-assets.com/46584437/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/26270402/Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral">Secuencias Sedimentarias del Rio Huaura - Sector Huaral</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a la altura del pueblo de Alcantarilla; esta zona corresponde al cuadrángulo de Huacho (23-h). La salida de campo realizó como parte de las actividades de la asignatura de sedimentología para consolidar nuestros conocimientos teóricos adquiridos y de este modo poder aplicar estos en campo. La zona estudiada durante la salida fue en la margen izquierda del rio Huaura del Albiano-Cenomaniano. En esta zona se observaron estructuras sobresalientes como dique y fallas sinsedementarias.<br /><br />Siguiendo con el recorrido, más al este se observaron sucesiones sedimentarias en su mayoría de grano decreciente, como también se observaron debris flow, contornitas uniformes, interbancos, diastemas y flujos de turbiditas. En esta zona de manera general de concluye que los flujos de alta densidad se concentran más a la base, donde los clastos son mucho más gruesos y conforme vamos subiendo en la secuencia sedimentaria, los que más predominan son los flujos de arena (sand flow).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="22a7e4f8c023336c5de29aa5990d3c8e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46584437,"asset_id":26270402,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46584437/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="26270402"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="26270402"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 26270402; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=26270402]").text(description); $(".js-view-count[data-work-id=26270402]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 26270402; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='26270402']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 26270402, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "22a7e4f8c023336c5de29aa5990d3c8e" } } $('.js-work-strip[data-work-id=26270402]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":26270402,"title":"Secuencias Sedimentarias del Rio Huaura - Sector Huaral","translated_title":"","metadata":{"abstract":"La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a la altura del pueblo de Alcantarilla; esta zona corresponde al cuadrángulo de Huacho (23-h). La salida de campo realizó como parte de las actividades de la asignatura de sedimentología para consolidar nuestros conocimientos teóricos adquiridos y de este modo poder aplicar estos en campo. La zona estudiada durante la salida fue en la margen izquierda del rio Huaura del Albiano-Cenomaniano. En esta zona se observaron estructuras sobresalientes como dique y fallas sinsedementarias.\n\nSiguiendo con el recorrido, más al este se observaron sucesiones sedimentarias en su mayoría de grano decreciente, como también se observaron debris flow, contornitas uniformes, interbancos, diastemas y flujos de turbiditas. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="24702513"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/24702513/Construcci%C3%B3n_de_un_t%C3%BAnel_trabajo_pr%C3%A1ctico"><img alt="Research paper thumbnail of Construcción de un túnel, trabajo práctico." class="work-thumbnail" src="https://attachments.academia-assets.com/45035317/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/24702513/Construcci%C3%B3n_de_un_t%C3%BAnel_trabajo_pr%C3%A1ctico">Construcción de un túnel, trabajo práctico.</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo topográfico de una poligonal abierta y la construcción de una obra de acuerdo a las especificaciones de la topo tarea, en este caso fue la construcción de dos túneles que no se llegan a unir y se desea calcular las coordenadas de todos los vértices de ambas poligonales abiertas y también el volumen a desplazar de tierra para que estos se conecten. Desarrollaremos una poligonal es una serie de líneas consecutivas cuyos extremos se han marcado en el campo, así como sus longitudes y direcciones se han determinado a partir de mediciones en el campo. Una poligonal abierta consta de una serie de líneas unidas, pero estas no regresan al punto de partida ni cierran en un punto con igual o mayor orden de exactitud.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="258b3aad65c5f76cda7a88b841f0eaf3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45035317,"asset_id":24702513,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45035317/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="24702513"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="24702513"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 24702513; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=24702513]").text(description); $(".js-view-count[data-work-id=24702513]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 24702513; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='24702513']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 24702513, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "258b3aad65c5f76cda7a88b841f0eaf3" } } $('.js-work-strip[data-work-id=24702513]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":24702513,"title":"Construcción de un túnel, trabajo práctico.","translated_title":"","metadata":{"abstract":"Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo topográfico de una poligonal abierta y la construcción de una obra de acuerdo a las especificaciones de la topo tarea, en este caso fue la construcción de dos túneles que no se llegan a unir y se desea calcular las coordenadas de todos los vértices de ambas poligonales abiertas y también el volumen a desplazar de tierra para que estos se conecten. 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Desarrollaremos una poligonal es una serie de líneas consecutivas cuyos extremos se han marcado en el campo, así como sus longitudes y direcciones se han determinado a partir de mediciones en el campo. 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Los pequeños lentes de ofiolitas ultramáficas, ahora desmembradas e incorporadas en los cinturones deformados de montañas, se denominan Peridotitas Alpinas.\n\nhttp://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/"},"translated_abstract":"Las Ofiolitas son definidas como grandes masas Máficas a ultramáficas tabulares, que se presume se han formado a partir de antigua corteza oceánica o del manto superior, que han sido falladas y transportadas como lentes en los continentes e incorporadas en los cinturones montañosos. Los pequeños lentes de ofiolitas ultramáficas, ahora desmembradas e incorporadas en los cinturones deformados de montañas, se denominan Peridotitas Alpinas.\n\nhttp://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/","internal_url":"https://www.academia.edu/23390749/Rocas_Igneas_de_Margenes_Continentales_Suite_Ofiolita","translated_internal_url":"","created_at":"2016-03-17T17:58:16.698-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30199075,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":17497236,"work_id":23390749,"tagging_user_id":30199075,"tagged_user_id":39491278,"co_author_invite_id":null,"email":"m***n@geoxnet.com","affiliation":"Universidad Nacional Mayor de San Marcos","display_order":0,"name":"Geo Xnet","title":"Rocas Igneas de Margenes Continentales - Suite Ofiolita"}],"downloadable_attachments":[{"id":43838468,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43838468/thumbnails/1.jpg","file_name":"Rocas_Igneas_de_Margenes_Continentales.pdf","download_url":"https://www.academia.edu/attachments/43838468/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rocas_Igneas_de_Margenes_Continentales_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43838468/Rocas_Igneas_de_Margenes_Continentales-libre.pdf?1458262505=\u0026response-content-disposition=attachment%3B+filename%3DRocas_Igneas_de_Margenes_Continentales_S.pdf\u0026Expires=1732438492\u0026Signature=GxyjOFGEJZrR8bKOrQdg786Ll3St2KjucsUUK2xvHiR6Z1RWWqnoON1pZBXR18UjGw26NHtrOV4bpY-msVUrgDFvsc79s-30R9yutvoMShLe~XCEx3dX1q6fpIZXbAcFBnhiRtNp3x-gSKYhxMpvp3JlWrHKw2mAjZYSAUgdRbborMMpMfqe62PLCjXL6~1-wiAivIJEihLDMX2EMCv26C9MfHDILRUAnxUnd43U7TbHv8p3kpH-n8GbVau3Jc4EtB1nrnfbepnW8XlJcgN0GDu5XLAKiueC27y1bg4OVSAO3SZ2BQ8eBBwccNM20xNbUjL59xMzlcnMRAgAapxTtg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Rocas_Igneas_de_Margenes_Continentales_Suite_Ofiolita","translated_slug":"","page_count":35,"language":"es","content_type":"Work","owner":{"id":30199075,"first_name":"Victor","middle_initials":"","last_name":"Medina","page_name":"VictorMedina_","domain_name":"independent","created_at":"2015-04-23T21:39:03.282-07:00","display_name":"Victor Medina","url":"https://independent.academia.edu/VictorMedina_"},"attachments":[{"id":43838468,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43838468/thumbnails/1.jpg","file_name":"Rocas_Igneas_de_Margenes_Continentales.pdf","download_url":"https://www.academia.edu/attachments/43838468/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rocas_Igneas_de_Margenes_Continentales_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43838468/Rocas_Igneas_de_Margenes_Continentales-libre.pdf?1458262505=\u0026response-content-disposition=attachment%3B+filename%3DRocas_Igneas_de_Margenes_Continentales_S.pdf\u0026Expires=1732438492\u0026Signature=GxyjOFGEJZrR8bKOrQdg786Ll3St2KjucsUUK2xvHiR6Z1RWWqnoON1pZBXR18UjGw26NHtrOV4bpY-msVUrgDFvsc79s-30R9yutvoMShLe~XCEx3dX1q6fpIZXbAcFBnhiRtNp3x-gSKYhxMpvp3JlWrHKw2mAjZYSAUgdRbborMMpMfqe62PLCjXL6~1-wiAivIJEihLDMX2EMCv26C9MfHDILRUAnxUnd43U7TbHv8p3kpH-n8GbVau3Jc4EtB1nrnfbepnW8XlJcgN0GDu5XLAKiueC27y1bg4OVSAO3SZ2BQ8eBBwccNM20xNbUjL59xMzlcnMRAgAapxTtg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology"},{"id":15989,"name":"Igneous petrology","url":"https://www.academia.edu/Documents/in/Igneous_petrology"},{"id":44747,"name":"Plate Tectonics","url":"https://www.academia.edu/Documents/in/Plate_Tectonics"},{"id":147519,"name":"Geologia","url":"https://www.academia.edu/Documents/in/Geologia"},{"id":280922,"name":"Petrologia","url":"https://www.academia.edu/Documents/in/Petrologia"},{"id":840750,"name":"Tectonica De Placas","url":"https://www.academia.edu/Documents/in/Tectonica_De_Placas"}],"urls":[{"id":6916125,"url":"http://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="21741158"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/21741158/Clasificaci%C3%B3n_Qu%C3%ADmica_de_las_Rocas_Igneas"><img alt="Research paper thumbnail of Clasificación Química de las Rocas Igneas" class="work-thumbnail" src="https://attachments.academia-assets.com/42502582/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/21741158/Clasificaci%C3%B3n_Qu%C3%ADmica_de_las_Rocas_Igneas">Clasificación Química de las Rocas Igneas</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma c...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. <br /><br />Los granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a5add7fd5b092b4e3ed1046fc1d3ae02" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":42502582,"asset_id":21741158,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/42502582/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="21741158"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="21741158"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 21741158; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=21741158]").text(description); $(".js-view-count[data-work-id=21741158]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 21741158; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='21741158']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 21741158, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a5add7fd5b092b4e3ed1046fc1d3ae02" } } $('.js-work-strip[data-work-id=21741158]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":21741158,"title":"Clasificación Química de las Rocas Igneas","translated_title":"","metadata":{"abstract":"Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. \n\nLos granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios. "},"translated_abstract":"Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. \n\nLos granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios. 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Trabajo Práctico de Gabinete Pirita, Calcopirita, Magnetita, Hem...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Microscopía de Minerales Opacos.<br />Trabajo Práctico de Gabinete<br />Pirita, Calcopirita, Magnetita, Hematita, Galena, Esfalerita, Bornonita, Platas Rojas, Bornita, Arsenopirita, Oro, Estibinita, Bismutinita, Tenantita, Tetraedrita, Covelita, Goetita, Estibina, Enargita, Wolframita, Cobre Nativo, Cuprita.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="28bf3d29d1a37fe22c93ea546a85de4f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":40521251,"asset_id":19252526,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/40521251/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="19252526"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="19252526"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 19252526; 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El cambio es esencialmente debido a una adaptación de la roca a condiciones físicas que difieren de aquellas bajo las que la roca parental se formó y que difieren de las condiciones físicas que normalmente existen en la superficie de la tierra y en la zona de diagénesis.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="eb77d4a6a4b9833ed1a510d80f4c0184" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39796602,"asset_id":17952923,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39796602/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="17952923"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17952923"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17952923; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17952923]").text(description); $(".js-view-count[data-work-id=17952923]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17952923; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17952923']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17952923, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "eb77d4a6a4b9833ed1a510d80f4c0184" } } $('.js-work-strip[data-work-id=17952923]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17952923,"title":"Metamorfismo: Tipos, Grados, Facies","translated_title":"","metadata":{"abstract":"Metamorfismo: Proceso que implica cambios en la mineralogía y/o microestructura de una roca en estado sólido. 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By Michel Demange. Traducción. </span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8e4c6d6ca40f6f7bc546aae2b5e8d3b4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39794029,"asset_id":17948176,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39794029/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="17948176"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17948176"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17948176; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="17231855"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/17231855/Humedales_de_Puerto_Viejo"><img alt="Research paper thumbnail of Humedales de Puerto Viejo" class="work-thumbnail" src="https://attachments.academia-assets.com/39395038/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/17231855/Humedales_de_Puerto_Viejo">Humedales de Puerto Viejo</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Los Humedales de Puerto Viejo también conocido como Puerto Viejo está ubicado en el kilometro 73 ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Los Humedales de Puerto Viejo también conocido como Puerto Viejo está ubicado en el kilometro 73 de la Panamericana Sur.  Partiendo de Lima aproximadamente a 45 minutos.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e9bbaba592a73034419d53306ad6bdc5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39395038,"asset_id":17231855,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39395038/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="17231855"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17231855"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17231855; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="2890526" id="papers"><div class="js-work-strip profile--work_container" data-work-id="29741804"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/29741804/PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN"><img alt="Research paper thumbnail of PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN" class="work-thumbnail" src="https://attachments.academia-assets.com/50198758/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/29741804/PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN: IMPLICATIONS FOR HYDROCARBON OCCURRENCE AT THE...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN: IMPLICATIONS FOR HYDROCARBON OCCURRENCE AT THE SOUTH LIBERTY SALT DOME<br /><br />Generación de Petróleo en la Cuenca Sureste de Texas:<br />Implicaciones para la ocurrencia de Hidrocarburos<br /> en el Domo Salino “South Liberty”<br /><br />Las Características Geoquímicas de Hidrocarburos del yacimiento “South Liberty”, condado Liberty-Texas, fueron integradas a la estratigrafía local, presión, temperatura, datos sísmicos y la química del agua para determinar su origen, madurez y vías de migración de hidrocarburos asociados con el Domo de Sal en el Sur-este de ”Texas Gulf Coast”.  Catorce muestras de aceite crudo fueron obtenidas de los reservorios de ligera-geopresurización "Cook Mountain" y "Yegua" (ambos del Eoceno) y "Frio" (Oligoceno) (189-2886 metros [3245-9469 pies]) fueron analizados mediante Cromatografía de Gases (GC) y Espectrometría de masas GC-mass.  Los datos de presión y temperatura de los 36 pozos fueron usados para modelar la historia de la maduración termal en las proximidades del domo.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2749c475adc602b07ea44aaa53c7bb79" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50198758,"asset_id":29741804,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50198758/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="29741804"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="29741804"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 29741804; 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Catorce muestras de aceite crudo fueron obtenidas de los reservorios de ligera-geopresurización \"Cook Mountain\" y \"Yegua\" (ambos del Eoceno) y \"Frio\" (Oligoceno) (189-2886 metros [3245-9469 pies]) fueron analizados mediante Cromatografía de Gases (GC) y Espectrometría de masas GC-mass. Los datos de presión y temperatura de los 36 pozos fueron usados para modelar la historia de la maduración termal en las proximidades del domo.\n"},"translated_abstract":"PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN: IMPLICATIONS FOR HYDROCARBON OCCURRENCE AT THE SOUTH LIBERTY SALT DOME\n\nGeneración de Petróleo en la Cuenca Sureste de Texas:\nImplicaciones para la ocurrencia de Hidrocarburos\n en el Domo Salino “South Liberty”\n\nLas Características Geoquímicas de Hidrocarburos del yacimiento “South Liberty”, condado Liberty-Texas, fueron integradas a la estratigrafía local, presión, temperatura, datos sísmicos y la química del agua para determinar su origen, madurez y vías de migración de hidrocarburos asociados con el Domo de Sal en el Sur-este de ”Texas Gulf Coast”. Catorce muestras de aceite crudo fueron obtenidas de los reservorios de ligera-geopresurización \"Cook Mountain\" y \"Yegua\" (ambos del Eoceno) y \"Frio\" (Oligoceno) (189-2886 metros [3245-9469 pies]) fueron analizados mediante Cromatografía de Gases (GC) y Espectrometría de masas GC-mass. Los datos de presión y temperatura de los 36 pozos fueron usados para modelar la historia de la maduración termal en las proximidades del domo.\n","internal_url":"https://www.academia.edu/29741804/PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN","translated_internal_url":"","created_at":"2016-11-08T18:13:37.382-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30199075,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":25814124,"work_id":29741804,"tagging_user_id":30199075,"tagged_user_id":39491278,"co_author_invite_id":null,"email":"m***n@geoxnet.com","affiliation":"Universidad Nacional Mayor de San Marcos","display_order":1,"name":"Geo Xnet","title":"PETROLEUM GENERATION IN THE SOUTHEAST TEXAS BASIN"}],"downloadable_attachments":[{"id":50198758,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50198758/thumbnails/1.jpg","file_name":"EXPO_Domo_South_Liberty.pdf","download_url":"https://www.academia.edu/attachments/50198758/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TE.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50198758/EXPO_Domo_South_Liberty-libre.pdf?1478659489=\u0026response-content-disposition=attachment%3B+filename%3DPETROLEUM_GENERATION_IN_THE_SOUTHEAST_TE.pdf\u0026Expires=1732438491\u0026Signature=E18WTwmBg3vgGgxDZ2QXoQpNDepJWJ2ymM0~6qqxumdk7FgQmuLvlyIzYRWkywf8NTxmH9N6xoNg07xmMgMMVwBEvb2Y2PUorQkcQgl4XujIgVLNnic1EatAA5rh6on6K48pz0CXjfpFveSp1tFKv3U3vs-TokqvetwOXhe8McPZbOpu2lRKjbbqHtoU2anDoV4MDHz7SSSySx1JWC6A-0tCl39571atpjepbk1s7QpRP2d9RoXQpSGSbdbZM0GZs67ss16zC-oycjt-Eazm351MEVozekklSmGZujCggu-rmVqDonA-lzMOpHnhL0RAYxsyEtFYK~5g8yWvKe-Apw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TEXAS_BASIN","translated_slug":"","page_count":31,"language":"es","content_type":"Work","owner":{"id":30199075,"first_name":"Victor","middle_initials":"","last_name":"Medina","page_name":"VictorMedina_","domain_name":"independent","created_at":"2015-04-23T21:39:03.282-07:00","display_name":"Victor Medina","url":"https://independent.academia.edu/VictorMedina_"},"attachments":[{"id":50198758,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50198758/thumbnails/1.jpg","file_name":"EXPO_Domo_South_Liberty.pdf","download_url":"https://www.academia.edu/attachments/50198758/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"PETROLEUM_GENERATION_IN_THE_SOUTHEAST_TE.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50198758/EXPO_Domo_South_Liberty-libre.pdf?1478659489=\u0026response-content-disposition=attachment%3B+filename%3DPETROLEUM_GENERATION_IN_THE_SOUTHEAST_TE.pdf\u0026Expires=1732438491\u0026Signature=E18WTwmBg3vgGgxDZ2QXoQpNDepJWJ2ymM0~6qqxumdk7FgQmuLvlyIzYRWkywf8NTxmH9N6xoNg07xmMgMMVwBEvb2Y2PUorQkcQgl4XujIgVLNnic1EatAA5rh6on6K48pz0CXjfpFveSp1tFKv3U3vs-TokqvetwOXhe8McPZbOpu2lRKjbbqHtoU2anDoV4MDHz7SSSySx1JWC6A-0tCl39571atpjepbk1s7QpRP2d9RoXQpSGSbdbZM0GZs67ss16zC-oycjt-Eazm351MEVozekklSmGZujCggu-rmVqDonA-lzMOpHnhL0RAYxsyEtFYK~5g8yWvKe-Apw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1034,"name":"Stratigraphy","url":"https://www.academia.edu/Documents/in/Stratigraphy"},{"id":5285,"name":"Petroleum","url":"https://www.academia.edu/Documents/in/Petroleum"},{"id":15989,"name":"Igneous petrology","url":"https://www.academia.edu/Documents/in/Igneous_petrology"},{"id":115560,"name":"Estratigrafía","url":"https://www.academia.edu/Documents/in/Estratigraf%C3%ADa"},{"id":266093,"name":"GEOLOGIA Y PETROLEO","url":"https://www.academia.edu/Documents/in/GEOLOGIA_Y_PETROLEO"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="26270402"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/26270402/Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral"><img alt="Research paper thumbnail of Secuencias Sedimentarias del Rio Huaura - Sector Huaral" class="work-thumbnail" src="https://attachments.academia-assets.com/46584437/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/26270402/Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral">Secuencias Sedimentarias del Rio Huaura - Sector Huaral</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a la altura del pueblo de Alcantarilla; esta zona corresponde al cuadrángulo de Huacho (23-h). La salida de campo realizó como parte de las actividades de la asignatura de sedimentología para consolidar nuestros conocimientos teóricos adquiridos y de este modo poder aplicar estos en campo. La zona estudiada durante la salida fue en la margen izquierda del rio Huaura del Albiano-Cenomaniano. En esta zona se observaron estructuras sobresalientes como dique y fallas sinsedementarias.<br /><br />Siguiendo con el recorrido, más al este se observaron sucesiones sedimentarias en su mayoría de grano decreciente, como también se observaron debris flow, contornitas uniformes, interbancos, diastemas y flujos de turbiditas. En esta zona de manera general de concluye que los flujos de alta densidad se concentran más a la base, donde los clastos son mucho más gruesos y conforme vamos subiendo en la secuencia sedimentaria, los que más predominan son los flujos de arena (sand flow).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="22a7e4f8c023336c5de29aa5990d3c8e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46584437,"asset_id":26270402,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46584437/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="26270402"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="26270402"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 26270402; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=26270402]").text(description); $(".js-view-count[data-work-id=26270402]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 26270402; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='26270402']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 26270402, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "22a7e4f8c023336c5de29aa5990d3c8e" } } $('.js-work-strip[data-work-id=26270402]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":26270402,"title":"Secuencias Sedimentarias del Rio Huaura - Sector Huaral","translated_title":"","metadata":{"abstract":"La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a la altura del pueblo de Alcantarilla; esta zona corresponde al cuadrángulo de Huacho (23-h). La salida de campo realizó como parte de las actividades de la asignatura de sedimentología para consolidar nuestros conocimientos teóricos adquiridos y de este modo poder aplicar estos en campo. La zona estudiada durante la salida fue en la margen izquierda del rio Huaura del Albiano-Cenomaniano. En esta zona se observaron estructuras sobresalientes como dique y fallas sinsedementarias.\n\nSiguiendo con el recorrido, más al este se observaron sucesiones sedimentarias en su mayoría de grano decreciente, como también se observaron debris flow, contornitas uniformes, interbancos, diastemas y flujos de turbiditas. En esta zona de manera general de concluye que los flujos de alta densidad se concentran más a la base, donde los clastos son mucho más gruesos y conforme vamos subiendo en la secuencia sedimentaria, los que más predominan son los flujos de arena (sand flow)."},"translated_abstract":"La zona de estudio se encuentra al norte de Lima, en la provincia de Huaura, distrito de Huaura a la altura del pueblo de Alcantarilla; esta zona corresponde al cuadrángulo de Huacho (23-h). La salida de campo realizó como parte de las actividades de la asignatura de sedimentología para consolidar nuestros conocimientos teóricos adquiridos y de este modo poder aplicar estos en campo. La zona estudiada durante la salida fue en la margen izquierda del rio Huaura del Albiano-Cenomaniano. En esta zona se observaron estructuras sobresalientes como dique y fallas sinsedementarias.\n\nSiguiendo con el recorrido, más al este se observaron sucesiones sedimentarias en su mayoría de grano decreciente, como también se observaron debris flow, contornitas uniformes, interbancos, diastemas y flujos de turbiditas. En esta zona de manera general de concluye que los flujos de alta densidad se concentran más a la base, donde los clastos son mucho más gruesos y conforme vamos subiendo en la secuencia sedimentaria, los que más predominan son los flujos de arena (sand flow).","internal_url":"https://www.academia.edu/26270402/Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral","translated_internal_url":"","created_at":"2016-06-17T20:59:37.961-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30199075,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":21441393,"work_id":26270402,"tagging_user_id":30199075,"tagged_user_id":39491278,"co_author_invite_id":null,"email":"m***n@geoxnet.com","affiliation":"Universidad Nacional Mayor de San Marcos","display_order":1,"name":"Geo Xnet","title":"Secuencias Sedimentarias del Rio Huaura - Sector Huaral"}],"downloadable_attachments":[{"id":46584437,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/46584437/thumbnails/1.jpg","file_name":"Secuencias_Sedimentarias_Huacho_FINAL.pdf","download_url":"https://www.academia.edu/attachments/46584437/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Secuencias_Sedimentarias_del_Rio_Huaura.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/46584437/Secuencias_Sedimentarias_Huacho_FINAL-libre.pdf?1466222332=\u0026response-content-disposition=attachment%3B+filename%3DSecuencias_Sedimentarias_del_Rio_Huaura.pdf\u0026Expires=1732438491\u0026Signature=SrvVqMnb2sO934TVsakxyHKq79KzSkN7OEvta25s6HVINkj90zi07gX~5May1RZC2W2qtj-UOBi-9MAGLIELMgQgMK2xEyy6QZ1GE5YLWSmZfiPlVxZBjYY6q8m1EaLihjyx-SYm5pFHgyh-7AgfvswkEZiTy5Zh8oo2Lb83PPHiU09xlSTxhJIkkw5z8PbVmz0YkKxm8JKf6fZrJF1fwCp3Y063Rbhx1EgHI5IL6PWvr97Fx4YSmD9vRj-D~mgl44DS5AT1EAsNLAjFWkhGSQKb1YWc--lUOT2L-1lF64UvZD8mDV-411~N2if0gh~KBe-ih6UXEva88A3gPqybrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Secuencias_Sedimentarias_del_Rio_Huaura_Sector_Huaral","translated_slug":"","page_count":22,"language":"es","content_type":"Work","owner":{"id":30199075,"first_name":"Victor","middle_initials":"","last_name":"Medina","page_name":"VictorMedina_","domain_name":"independent","created_at":"2015-04-23T21:39:03.282-07:00","display_name":"Victor Medina","url":"https://independent.academia.edu/VictorMedina_"},"attachments":[{"id":46584437,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/46584437/thumbnails/1.jpg","file_name":"Secuencias_Sedimentarias_Huacho_FINAL.pdf","download_url":"https://www.academia.edu/attachments/46584437/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Secuencias_Sedimentarias_del_Rio_Huaura.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/46584437/Secuencias_Sedimentarias_Huacho_FINAL-libre.pdf?1466222332=\u0026response-content-disposition=attachment%3B+filename%3DSecuencias_Sedimentarias_del_Rio_Huaura.pdf\u0026Expires=1732438491\u0026Signature=SrvVqMnb2sO934TVsakxyHKq79KzSkN7OEvta25s6HVINkj90zi07gX~5May1RZC2W2qtj-UOBi-9MAGLIELMgQgMK2xEyy6QZ1GE5YLWSmZfiPlVxZBjYY6q8m1EaLihjyx-SYm5pFHgyh-7AgfvswkEZiTy5Zh8oo2Lb83PPHiU09xlSTxhJIkkw5z8PbVmz0YkKxm8JKf6fZrJF1fwCp3Y063Rbhx1EgHI5IL6PWvr97Fx4YSmD9vRj-D~mgl44DS5AT1EAsNLAjFWkhGSQKb1YWc--lUOT2L-1lF64UvZD8mDV-411~N2if0gh~KBe-ih6UXEva88A3gPqybrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":420,"name":"Sedimentology","url":"https://www.academia.edu/Documents/in/Sedimentology"},{"id":48807,"name":"Sedimentary geology and stratigraphy","url":"https://www.academia.edu/Documents/in/Sedimentary_geology_and_stratigraphy"},{"id":719873,"name":"Huaura y Huacho en Perú","url":"https://www.academia.edu/Documents/in/Huaura_y_Huacho_en_Peru"},{"id":1008094,"name":"Huaral","url":"https://www.academia.edu/Documents/in/Huaral"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="25054832"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/25054832/Magmas"><img alt="Research paper thumbnail of Magmas" class="work-thumbnail" src="https://attachments.academia-assets.com/45377007/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/25054832/Magmas">Magmas</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Límitedeplacaslitosféricas Mantosuperiordeperidotita Densidad Viscosidad Ambientetectónico Geomet...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Límitedeplacaslitosféricas<br />Mantosuperiordeperidotita<br />Densidad<br />Viscosidad<br />Ambientetectónico<br />Geometría,volumendelcuerpo<br />Conductos</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a9a5c066f69601904ea35aba7dc35ebb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45377007,"asset_id":25054832,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45377007/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="25054832"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="25054832"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25054832; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="24702513"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/24702513/Construcci%C3%B3n_de_un_t%C3%BAnel_trabajo_pr%C3%A1ctico"><img alt="Research paper thumbnail of Construcción de un túnel, trabajo práctico." class="work-thumbnail" src="https://attachments.academia-assets.com/45035317/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/24702513/Construcci%C3%B3n_de_un_t%C3%BAnel_trabajo_pr%C3%A1ctico">Construcción de un túnel, trabajo práctico.</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo topográfico de una poligonal abierta y la construcción de una obra de acuerdo a las especificaciones de la topo tarea, en este caso fue la construcción de dos túneles que no se llegan a unir y se desea calcular las coordenadas de todos los vértices de ambas poligonales abiertas y también el volumen a desplazar de tierra para que estos se conecten. Desarrollaremos una poligonal es una serie de líneas consecutivas cuyos extremos se han marcado en el campo, así como sus longitudes y direcciones se han determinado a partir de mediciones en el campo. Una poligonal abierta consta de una serie de líneas unidas, pero estas no regresan al punto de partida ni cierran en un punto con igual o mayor orden de exactitud.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="258b3aad65c5f76cda7a88b841f0eaf3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45035317,"asset_id":24702513,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45035317/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="24702513"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="24702513"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 24702513; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=24702513]").text(description); $(".js-view-count[data-work-id=24702513]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 24702513; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='24702513']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 24702513, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "258b3aad65c5f76cda7a88b841f0eaf3" } } $('.js-work-strip[data-work-id=24702513]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":24702513,"title":"Construcción de un túnel, trabajo práctico.","translated_title":"","metadata":{"abstract":"Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo topográfico de una poligonal abierta y la construcción de una obra de acuerdo a las especificaciones de la topo tarea, en este caso fue la construcción de dos túneles que no se llegan a unir y se desea calcular las coordenadas de todos los vértices de ambas poligonales abiertas y también el volumen a desplazar de tierra para que estos se conecten. Desarrollaremos una poligonal es una serie de líneas consecutivas cuyos extremos se han marcado en el campo, así como sus longitudes y direcciones se han determinado a partir de mediciones en el campo. Una poligonal abierta consta de una serie de líneas unidas, pero estas no regresan al punto de partida ni cierran en un punto con igual o mayor orden de exactitud."},"translated_abstract":"Este trabajo se ha elaborado con la finalidad de dar a conocer cómo se puede realizar un trabajo topográfico de una poligonal abierta y la construcción de una obra de acuerdo a las especificaciones de la topo tarea, en este caso fue la construcción de dos túneles que no se llegan a unir y se desea calcular las coordenadas de todos los vértices de ambas poligonales abiertas y también el volumen a desplazar de tierra para que estos se conecten. Desarrollaremos una poligonal es una serie de líneas consecutivas cuyos extremos se han marcado en el campo, así como sus longitudes y direcciones se han determinado a partir de mediciones en el campo. Una poligonal abierta consta de una serie de líneas unidas, pero estas no regresan al punto de partida ni cierran en un punto con igual o mayor orden de exactitud.","internal_url":"https://www.academia.edu/24702513/Construcci%C3%B3n_de_un_t%C3%BAnel_trabajo_pr%C3%A1ctico","translated_internal_url":"","created_at":"2016-04-24T00:27:58.261-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30199075,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":45035317,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/45035317/thumbnails/1.jpg","file_name":"Construccion_de_un_tunel.pdf","download_url":"https://www.academia.edu/attachments/45035317/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Construccion_de_un_tunel_trabajo_practic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/45035317/Construccion_de_un_tunel-libre.pdf?1461482794=\u0026response-content-disposition=attachment%3B+filename%3DConstruccion_de_un_tunel_trabajo_practic.pdf\u0026Expires=1732438492\u0026Signature=b6TEmSxswtUcmQ8pnErKKLd5cPOa-kY~8ZGmBdPGPU842ox-OREZ1wq02OepkiqrOiZlNjCS39e7q-rehz~e9-m6TX3KlPQBCMqgcGuviXMQi5~BnHR2fjb4yNozlOvAaCSAXTQJqJdK0tumyT9h1BlDcyEyLqJ9dLHyJsPRm6faaz3DOs4gWDbd-DbFIpgdS7Uat5BMlAN-yP9si3RK3o-Zq9xqDMtAUlm6NfTzC5~SuJ0AAhd~FqmYZvAmlWD2SZiIEaqK~lsFBBzjw92eyq1d7QrIpoUfR199ED0ur2u6zX1jlaF8fJ1jw1Aasg6ZsDFluBRmBdwmIs8tFXWCCA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Construcción_de_un_túnel_trabajo_práctico","translated_slug":"","page_count":16,"language":"es","content_type":"Work","owner":{"id":30199075,"first_name":"Victor","middle_initials":"","last_name":"Medina","page_name":"VictorMedina_","domain_name":"independent","created_at":"2015-04-23T21:39:03.282-07:00","display_name":"Victor Medina","url":"https://independent.academia.edu/VictorMedina_"},"attachments":[{"id":45035317,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/45035317/thumbnails/1.jpg","file_name":"Construccion_de_un_tunel.pdf","download_url":"https://www.academia.edu/attachments/45035317/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Construccion_de_un_tunel_trabajo_practic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/45035317/Construccion_de_un_tunel-libre.pdf?1461482794=\u0026response-content-disposition=attachment%3B+filename%3DConstruccion_de_un_tunel_trabajo_practic.pdf\u0026Expires=1732438492\u0026Signature=b6TEmSxswtUcmQ8pnErKKLd5cPOa-kY~8ZGmBdPGPU842ox-OREZ1wq02OepkiqrOiZlNjCS39e7q-rehz~e9-m6TX3KlPQBCMqgcGuviXMQi5~BnHR2fjb4yNozlOvAaCSAXTQJqJdK0tumyT9h1BlDcyEyLqJ9dLHyJsPRm6faaz3DOs4gWDbd-DbFIpgdS7Uat5BMlAN-yP9si3RK3o-Zq9xqDMtAUlm6NfTzC5~SuJ0AAhd~FqmYZvAmlWD2SZiIEaqK~lsFBBzjw92eyq1d7QrIpoUfR199ED0ur2u6zX1jlaF8fJ1jw1Aasg6ZsDFluBRmBdwmIs8tFXWCCA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":333230,"name":"Topografia","url":"https://www.academia.edu/Documents/in/Topografia"},{"id":834991,"name":"Tuneles","url":"https://www.academia.edu/Documents/in/Tuneles"}],"urls":[]}, dispatcherData: dispatcherData }); 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Los pequeños lentes de ofiolitas ultramáficas, ahora desmembradas e incorporadas en los cinturones deformados de montañas, se denominan Peridotitas Alpinas.\n\nhttp://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/"},"translated_abstract":"Las Ofiolitas son definidas como grandes masas Máficas a ultramáficas tabulares, que se presume se han formado a partir de antigua corteza oceánica o del manto superior, que han sido falladas y transportadas como lentes en los continentes e incorporadas en los cinturones montañosos. Los pequeños lentes de ofiolitas ultramáficas, ahora desmembradas e incorporadas en los cinturones deformados de montañas, se denominan Peridotitas Alpinas.\n\nhttp://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/","internal_url":"https://www.academia.edu/23390749/Rocas_Igneas_de_Margenes_Continentales_Suite_Ofiolita","translated_internal_url":"","created_at":"2016-03-17T17:58:16.698-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":30199075,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":17497236,"work_id":23390749,"tagging_user_id":30199075,"tagged_user_id":39491278,"co_author_invite_id":null,"email":"m***n@geoxnet.com","affiliation":"Universidad Nacional Mayor de San Marcos","display_order":0,"name":"Geo Xnet","title":"Rocas Igneas de Margenes Continentales - Suite Ofiolita"}],"downloadable_attachments":[{"id":43838468,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43838468/thumbnails/1.jpg","file_name":"Rocas_Igneas_de_Margenes_Continentales.pdf","download_url":"https://www.academia.edu/attachments/43838468/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rocas_Igneas_de_Margenes_Continentales_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43838468/Rocas_Igneas_de_Margenes_Continentales-libre.pdf?1458262505=\u0026response-content-disposition=attachment%3B+filename%3DRocas_Igneas_de_Margenes_Continentales_S.pdf\u0026Expires=1732438492\u0026Signature=GxyjOFGEJZrR8bKOrQdg786Ll3St2KjucsUUK2xvHiR6Z1RWWqnoON1pZBXR18UjGw26NHtrOV4bpY-msVUrgDFvsc79s-30R9yutvoMShLe~XCEx3dX1q6fpIZXbAcFBnhiRtNp3x-gSKYhxMpvp3JlWrHKw2mAjZYSAUgdRbborMMpMfqe62PLCjXL6~1-wiAivIJEihLDMX2EMCv26C9MfHDILRUAnxUnd43U7TbHv8p3kpH-n8GbVau3Jc4EtB1nrnfbepnW8XlJcgN0GDu5XLAKiueC27y1bg4OVSAO3SZ2BQ8eBBwccNM20xNbUjL59xMzlcnMRAgAapxTtg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Rocas_Igneas_de_Margenes_Continentales_Suite_Ofiolita","translated_slug":"","page_count":35,"language":"es","content_type":"Work","owner":{"id":30199075,"first_name":"Victor","middle_initials":"","last_name":"Medina","page_name":"VictorMedina_","domain_name":"independent","created_at":"2015-04-23T21:39:03.282-07:00","display_name":"Victor Medina","url":"https://independent.academia.edu/VictorMedina_"},"attachments":[{"id":43838468,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43838468/thumbnails/1.jpg","file_name":"Rocas_Igneas_de_Margenes_Continentales.pdf","download_url":"https://www.academia.edu/attachments/43838468/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rocas_Igneas_de_Margenes_Continentales_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43838468/Rocas_Igneas_de_Margenes_Continentales-libre.pdf?1458262505=\u0026response-content-disposition=attachment%3B+filename%3DRocas_Igneas_de_Margenes_Continentales_S.pdf\u0026Expires=1732438492\u0026Signature=GxyjOFGEJZrR8bKOrQdg786Ll3St2KjucsUUK2xvHiR6Z1RWWqnoON1pZBXR18UjGw26NHtrOV4bpY-msVUrgDFvsc79s-30R9yutvoMShLe~XCEx3dX1q6fpIZXbAcFBnhiRtNp3x-gSKYhxMpvp3JlWrHKw2mAjZYSAUgdRbborMMpMfqe62PLCjXL6~1-wiAivIJEihLDMX2EMCv26C9MfHDILRUAnxUnd43U7TbHv8p3kpH-n8GbVau3Jc4EtB1nrnfbepnW8XlJcgN0GDu5XLAKiueC27y1bg4OVSAO3SZ2BQ8eBBwccNM20xNbUjL59xMzlcnMRAgAapxTtg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology"},{"id":15989,"name":"Igneous petrology","url":"https://www.academia.edu/Documents/in/Igneous_petrology"},{"id":44747,"name":"Plate Tectonics","url":"https://www.academia.edu/Documents/in/Plate_Tectonics"},{"id":147519,"name":"Geologia","url":"https://www.academia.edu/Documents/in/Geologia"},{"id":280922,"name":"Petrologia","url":"https://www.academia.edu/Documents/in/Petrologia"},{"id":840750,"name":"Tectonica De Placas","url":"https://www.academia.edu/Documents/in/Tectonica_De_Placas"}],"urls":[{"id":6916125,"url":"http://post.geoxnet.com/blog/rocas-igneas-de-margenes-continentales-la-suite-ofiolita/"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="21741158"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/21741158/Clasificaci%C3%B3n_Qu%C3%ADmica_de_las_Rocas_Igneas"><img alt="Research paper thumbnail of Clasificación Química de las Rocas Igneas" class="work-thumbnail" src="https://attachments.academia-assets.com/42502582/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/21741158/Clasificaci%C3%B3n_Qu%C3%ADmica_de_las_Rocas_Igneas">Clasificación Química de las Rocas Igneas</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma c...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. <br /><br />Los granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a5add7fd5b092b4e3ed1046fc1d3ae02" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":42502582,"asset_id":21741158,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/42502582/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="21741158"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="21741158"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 21741158; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=21741158]").text(description); $(".js-view-count[data-work-id=21741158]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 21741158; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='21741158']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 21741158, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a5add7fd5b092b4e3ed1046fc1d3ae02" } } $('.js-work-strip[data-work-id=21741158]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":21741158,"title":"Clasificación Química de las Rocas Igneas","translated_title":"","metadata":{"abstract":"Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. \n\nLos granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios. "},"translated_abstract":"Debido a que las rocas ígneas cristalizan a partir del magma, es conveniente pensar en el magma como un líquido que puede llegar a saturarse con un mineral en particular, lo que resulta es la cristalización de ese mineral. Normas químicas especifican que estos líquidos ordinariamente no pueden contener más de una cierta cantidad de un componente particular disuelto a una temperatura y presión dadas. Si al enfriar el magma se satura con un componente mineral en particular, entonces ese mineral se van a precipitar en forma de cristales y ser parte de la roca resultante. Este concepto es comúnmente aplicado a la sílice y minerales de sílice (usualmente cuarzo) en una amplia variedad de rocas ígneas de basaltos a granitoides. \n\nLos granitos son definidos en el sistema de clasificación del IUGS como rocas que contienen entre 20 y 60% de cuarzo y en el que feldespato alcalino constituye más del 35 % de la feldespato total. Sin embargo, los petrólogos han descubierto que las rocas magmáticas que se ajustan a este criterio mineralógico pueden tener contenidos muy variables de Al2O3, como se refleja en el contenido menor o minerales accesorios. 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Trabajo Práctico de Gabinete Pirita, Calcopirita, Magnetita, Hem...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Microscopía de Minerales Opacos.<br />Trabajo Práctico de Gabinete<br />Pirita, Calcopirita, Magnetita, Hematita, Galena, Esfalerita, Bornonita, Platas Rojas, Bornita, Arsenopirita, Oro, Estibinita, Bismutinita, Tenantita, Tetraedrita, Covelita, Goetita, Estibina, Enargita, Wolframita, Cobre Nativo, Cuprita.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="28bf3d29d1a37fe22c93ea546a85de4f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":40521251,"asset_id":19252526,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/40521251/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="19252526"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="19252526"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 19252526; 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By Michel Demange. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="17231855"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/17231855/Humedales_de_Puerto_Viejo"><img alt="Research paper thumbnail of Humedales de Puerto Viejo" class="work-thumbnail" src="https://attachments.academia-assets.com/39395038/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/17231855/Humedales_de_Puerto_Viejo">Humedales de Puerto Viejo</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Los Humedales de Puerto Viejo también conocido como Puerto Viejo está ubicado en el kilometro 73 ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Los Humedales de Puerto Viejo también conocido como Puerto Viejo está ubicado en el kilometro 73 de la Panamericana Sur.  Partiendo de Lima aproximadamente a 45 minutos.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e9bbaba592a73034419d53306ad6bdc5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39395038,"asset_id":17231855,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39395038/download_file?st=MTczMjQ0MDYyNCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="17231855"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17231855"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17231855; 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