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Classification","url":"https://www.academia.edu/Documents/in/Pattern_Classification?f_ri=409"},{"id":557803,"name":"Self Organized Map","url":"https://www.academia.edu/Documents/in/Self_Organized_Map?f_ri=409"},{"id":2226477,"name":"Automatic data processing","url":"https://www.academia.edu/Documents/in/Automatic_data_processing?f_ri=409"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_9996711" data-work_id="9996711" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/9996711/Experimental_Study_on_Radiometric_Performance_of_Synthetic_Aperture_Radiometer_HUT2D_Measurements_of_Natural_Targets">Experimental Study on Radiometric Performance of Synthetic Aperture Radiometer HUT2D—Measurements of Natural Targets</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This paper describes the analysis of L-band radiometric measurement data gathered with the synthetic aperture radiometer HUT-2D during several ground-based and airborne measurement campaigns. The radiometric data are analyzed from the... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_9996711" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This paper describes the analysis of L-band radiometric measurement data gathered with the synthetic aperture radiometer HUT-2D during several ground-based and airborne measurement campaigns. The radiometric data are analyzed from the instrument's performance point of view, aiming to verify the theoretical performance of an instrument of this kind and to assess the performance of the HUT-2D radiometer system in particular. The data sets considered for the study consist of measurements of well-known natural targets, such as cosmic background radiation, and measurements of pure water scenes, the brightness temperature of which is possible to model based on in situ measurements. We define four figures of merit, which are applicable for synthetic aperture radiometers. These are radiometric resolution, image bias, pixel-to-pixel random error, and temporal stability. Then, we use the selected data sets to assess these in the case of HUT-2D. The experimental results are discussed and compared to the theoretical values, where applicable. Also, we discuss possibilities to improve the presented performance. The main results of this paper are the consolidated performance parameters of the HUT-2D instrument. We study and discuss the properties of the error components related to the technology in a general level, and study the scalability of the errors as a function of the measured targets. In particular, the stability of the direction-dependent error component is pointed out, and a mitigation guideline is proposed.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/9996711" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="17e95c7d98aa8f8f83c445602aaa90b9" rel="nofollow" data-download="{"attachment_id":47576439,"asset_id":9996711,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/47576439/download_file?st=MTczMjQ1Mjc3OCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="24320359" href="https://independent.academia.edu/AliaAmira1">Alia Amira</a><script data-card-contents-for-user="24320359" type="text/json">{"id":24320359,"first_name":"Alia","last_name":"Amira","domain_name":"independent","page_name":"AliaAmira1","display_name":"Alia Amira","profile_url":"https://independent.academia.edu/AliaAmira1?f_ri=409","photo":"https://0.academia-photos.com/24320359/8572615/9577087/s65_alia.amira.jpg_oh_8cf77dc7937b09f06826be5bed94b9c0_oe_55e528ba___gda___1436675164_7b6cbead451441ca3c79dc98a3b05b4a"}</script></span></span></li><li class="js-paper-rank-work_9996711 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="9996711"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 9996711, container: ".js-paper-rank-work_9996711", }); 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The radiometric data are analyzed from the instrument's performance point of view, aiming to verify the theoretical performance of an instrument of this kind and to assess the performance of the HUT-2D radiometer system in particular. The data sets considered for the study consist of measurements of well-known natural targets, such as cosmic background radiation, and measurements of pure water scenes, the brightness temperature of which is possible to model based on in situ measurements. We define four figures of merit, which are applicable for synthetic aperture radiometers. These are radiometric resolution, image bias, pixel-to-pixel random error, and temporal stability. Then, we use the selected data sets to assess these in the case of HUT-2D. The experimental results are discussed and compared to the theoretical values, where applicable. Also, we discuss possibilities to improve the presented performance. The main results of this paper are the consolidated performance parameters of the HUT-2D instrument. We study and discuss the properties of the error components related to the technology in a general level, and study the scalability of the errors as a function of the measured targets. 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shelf","url":"https://www.academia.edu/Documents/in/Continental_shelf?f_ri=409"},{"id":415329,"name":"Subduction Zone","url":"https://www.academia.edu/Documents/in/Subduction_Zone?f_ri=409"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_14942992" data-work_id="14942992" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/14942992/Carbonatite_like_dykes_from_the_eastern_Himalayan_syntaxis_geochemical_isotopic_and_petrogenetic_evidence_for_melting_of_metasedimentary_carbonate_rocks_within_the_orogenic_crust">Carbonatite-like dykes from the eastern Himalayan syntaxis: geochemical, isotopic, and petrogenetic evidence for melting of metasedimentary carbonate rocks within the orogenic crust</a></div></div><div class="u-pb4x 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Analysis","url":"https://www.academia.edu/Documents/in/Data_Analysis?f_ri=409","nofollow":false},{"id":60580,"name":"Ionosphere","url":"https://www.academia.edu/Documents/in/Ionosphere?f_ri=409","nofollow":false},{"id":64388,"name":"Electromagnetic Waves","url":"https://www.academia.edu/Documents/in/Electromagnetic_Waves?f_ri=409","nofollow":false},{"id":65325,"name":"Electrical Circuit Theory","url":"https://www.academia.edu/Documents/in/Electrical_Circuit_Theory?f_ri=409"},{"id":80657,"name":"Surveys","url":"https://www.academia.edu/Documents/in/Surveys?f_ri=409"},{"id":153168,"name":"Data Collection","url":"https://www.academia.edu/Documents/in/Data_Collection?f_ri=409"},{"id":321836,"name":"Spectrum","url":"https://www.academia.edu/Documents/in/Spectrum?f_ri=409"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_38104819 coauthored" data-work_id="38104819" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/38104819/Regularization_of_P_P_and_P_S_converted_waves_data_through_the_FO_CRS_traveltime_approximation">Regularization of P-P and P-S converted waves data through the FO-CRS traveltime approximation</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">We present a new method of regularization of seismic data using the finite offset common reflection source (FOCRS) traveltime approximation. This method fits curves of common reflection source to the reflection events and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_38104819" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">We  present  a  new  method  of  regularization  of  seismic <br />data using the finite offset common reflection source (FOCRS)  traveltime  approximation.  This method fits  curves <br />of common  reflection source to the reflection events and <br />stacks all the amplitudes in a given aperture. The stacked <br />amplitude, afterwards, is allocated to the time coordinate <br />in the trace to be interpolated. We applied this method to<br />three  synthetic  velocity  models  and  the  results  showed <br />the capability for regularizing  converted seismic waves in <br />stratified medium.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/38104819" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="f7382a0b00090f9158e2e04285385e9d" rel="nofollow" data-download="{"attachment_id":58133513,"asset_id":38104819,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/58133513/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="2780675" href="https://independent.academia.edu/RaphaelDiCarlo">Raphael Di Carlo</a><script data-card-contents-for-user="2780675" type="text/json">{"id":2780675,"first_name":"Raphael","last_name":"Di Carlo","domain_name":"independent","page_name":"RaphaelDiCarlo","display_name":"Raphael Di Carlo","profile_url":"https://independent.academia.edu/RaphaelDiCarlo?f_ri=409","photo":"https://0.academia-photos.com/2780675/907606/21099251/s65_raphael.di_carlo.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-38104819">+1</span><div class="hidden js-additional-users-38104819"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/Jo%C3%A3oCarlosRibeiroCruz">João Carlos Ribeiro Cruz</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-38104819'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-38104819').html(); 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This method fits curves \nof common reflection source to the reflection events and \nstacks all the amplitudes in a given aperture. The stacked \namplitude, afterwards, is allocated to the time coordinate \nin the trace to be interpolated. We applied this method to\nthree synthetic velocity models and the results showed \nthe capability for regularizing converted seismic waves in \nstratified medium.","downloadable_attachments":[{"id":58133513,"asset_id":38104819,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":2780675,"first_name":"Raphael","last_name":"Di Carlo","domain_name":"independent","page_name":"RaphaelDiCarlo","display_name":"Raphael Di Carlo","profile_url":"https://independent.academia.edu/RaphaelDiCarlo?f_ri=409","photo":"https://0.academia-photos.com/2780675/907606/21099251/s65_raphael.di_carlo.jpg"},{"id":12143756,"first_name":"João Carlos Ribeiro","last_name":"Cruz","domain_name":"independent","page_name":"JoãoCarlosRibeiroCruz","display_name":"João Carlos Ribeiro 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type="text/json">{"id":20099,"name":"Sensitivity Analysis","url":"https://www.academia.edu/Documents/in/Sensitivity_Analysis?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="241558" href="https://www.academia.edu/Documents/in/Gulf_of_Mexico">Gulf of Mexico</a><script data-card-contents-for-ri="241558" type="text/json">{"id":241558,"name":"Gulf of Mexico","url":"https://www.academia.edu/Documents/in/Gulf_of_Mexico?f_ri=409","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=13849814]'), work: {"id":13849814,"title":"AVA simultaneous inversion of partially stacked seismic amplitude data for the spatial delineation of lithology and fluid units of deepwater hydrocarbon reservoirs in the central Gulf of 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href="https://www.academia.edu/Documents/in/Geophysics">Geophysics</a>, <script data-card-contents-for-ri="409" type="text/json">{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="17263" href="https://www.academia.edu/Documents/in/IOCG_Deposits">IOCG Deposits</a>, <script data-card-contents-for-ri="17263" type="text/json">{"id":17263,"name":"IOCG Deposits","url":"https://www.academia.edu/Documents/in/IOCG_Deposits?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="24963" href="https://www.academia.edu/Documents/in/Exploration_Geophysics">Exploration Geophysics</a>, <script data-card-contents-for-ri="24963" type="text/json">{"id":24963,"name":"Exploration Geophysics","url":"https://www.academia.edu/Documents/in/Exploration_Geophysics?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="70416" href="https://www.academia.edu/Documents/in/Mineral_exploration">Mineral exploration</a><script data-card-contents-for-ri="70416" type="text/json">{"id":70416,"name":"Mineral exploration","url":"https://www.academia.edu/Documents/in/Mineral_exploration?f_ri=409","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=7910446]'), work: {"id":7910446,"title":"UNDERSTANDING IRON OXIDE COPPER-GOLD (IOCG) MAGNETIC TARGETS FROM THE INSIDE OUT: CASE STUDIES FROM NORTHERN 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class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/14973107/Volcanology_Lessons_learned_from_Synthetic_Aperture_Radar_imagery">Volcanology: Lessons learned from Synthetic Aperture Radar imagery</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Twenty years of continuous Earth observation by satellite SAR have resulted in numerous new insights into active volcanism, including a better understanding of subsurface magma storage and transport, deposition of volcanic materials on... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_14973107" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Twenty years of continuous Earth observation by satellite SAR have resulted in numerous new insights into active volcanism, including a better understanding of subsurface magma storage and transport, deposition of volcanic materials on the surface, and the structure and development of volcanic edifices. This massive archive of data has resulted in fundamental leaps in our understanding of how volcanoes work - for example, identifying magma accumulation at supposedly quiescent volcanoes, even in remote areas or in the absence of ground-based data. In addition, global compilations of volcanic activity facilitate comparison of deformation behavior between different volcanic arcs and statistical evaluation of the strong link between deformation and eruption. SAR data are also increasingly used in timely hazard evaluation thanks to decreases in data latency and growth in processing and analysis techniques. The existing archive of SAR imagery is on the cusp of being enhanced by a new gene...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/14973107" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="1f52b3160d8791784351300c613b68ae" rel="nofollow" data-download="{"attachment_id":43685452,"asset_id":14973107,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/43685452/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="33968415" href="https://leeds.academia.edu/AndyHooper">Andy Hooper</a><script data-card-contents-for-user="33968415" type="text/json">{"id":33968415,"first_name":"Andy","last_name":"Hooper","domain_name":"leeds","page_name":"AndyHooper","display_name":"Andy Hooper","profile_url":"https://leeds.academia.edu/AndyHooper?f_ri=409","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_14973107 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="14973107"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 14973107, container: ".js-paper-rank-work_14973107", }); 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class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="8532383" href="https://independent.academia.edu/JamesMcCalpin">James McCalpin</a><script data-card-contents-for-user="8532383" type="text/json">{"id":8532383,"first_name":"James","last_name":"McCalpin","domain_name":"independent","page_name":"JamesMcCalpin","display_name":"James McCalpin","profile_url":"https://independent.academia.edu/JamesMcCalpin?f_ri=409","photo":"/images/s65_no_pic.png"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-14132638">+1</span><div class="hidden js-additional-users-14132638"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://humboldt.academia.edu/GaryCarver">Gary Carver</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-14132638'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-14132638').html(); } } new HoverPopover(popoverSettings); })();</script></li><li class="js-paper-rank-work_14132638 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="14132638"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 14132638, container: ".js-paper-rank-work_14132638", }); });</script></li><li class="js-percentile-work_14132638 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x 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})();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_10115613" data-work_id="10115613" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/10115613/Earth_electricity_a_review_of_mechanisms_which_cause_telluric_currents_in_the_lithosphere">Earth electricity: a review of mechanisms which cause telluric currents in the lithosphere</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Telluric currents are natural electrical phenomena in the Earth or its bodies of water. The strongest electric currents are related to lightning phenomena or space weather. Earth electricity can cause damage to structures, and may be... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_10115613" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Telluric currents are natural electrical phenomena in the Earth or its bodies of water. The strongest electric currents are related to lightning phenomena or space weather. Earth electricity can cause damage to structures, and may be useful for earthquake forecasting and other applications. Thirty-two distinct mechanisms that cause Earth electricity are<br />described, and a broad selection of current research is highlighted.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/10115613" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="db916eb35fd2b1add1a6c1f0470a3e6f" rel="nofollow" data-download="{"attachment_id":36233169,"asset_id":10115613,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/36233169/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="11839185" href="https://atpvp.academia.edu/DanielHelman">Daniel S Helman</a><script data-card-contents-for-user="11839185" type="text/json">{"id":11839185,"first_name":"Daniel","last_name":"Helman","domain_name":"atpvp","page_name":"DanielHelman","display_name":"Daniel S Helman","profile_url":"https://atpvp.academia.edu/DanielHelman?f_ri=409","photo":"https://0.academia-photos.com/11839185/3443802/4048663/s65_daniel.helman.jpg"}</script></span></span></li><li class="js-paper-rank-work_10115613 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="10115613"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 10115613, container: ".js-paper-rank-work_10115613", }); 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Early medieval enclosure at Glanfred, near Llandre, Ceredigion. Archaeologia Cambrensis 167: 221-243. Geophysical survey and small-scale trial... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_37506926" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Jones, I., Williams, D., Wiliams, S., Carruthers, W., Madgwick, R. and Young, T. 2018. Early medieval enclosure at Glanfred, near Llandre, Ceredigion. Archaeologia Cambrensis 167: 221-243. <br /><br />Geophysical survey and small-scale trial excavations were carried out on a small parchmark enclosure at Glanfred, near Llandre, Ceredigion in 2013. Geophysical survey revealed sections of the enclosure ditch that had not been previously visible from aerial photography, a number of possible entrances and two concentrations of internal anomalies. Excavation targeted a section of the inner of two ditches on the eastern side of the enclosure and an anomaly within the enclosure. An in situ iron slag deposit was discovered with an associated context dated between the late seventh and ninth century AD, whilst charred oats discovered in one of the lower deposits within the ditch was dated between the mid-fifth to sixth centuries AD. The results provide a rare insight into early medieval use of enclosures during the post-Roman and early medieval period, not only in northwest Ceredigion but more generally in Wales.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/37506926" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="f7f17ffeac6eed7ba155055b88c8d1d6" rel="nofollow" data-download="{"attachment_id":57478829,"asset_id":37506926,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/57478829/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="649778" href="https://cardiff.academia.edu/RichardMadgwick">Richard Madgwick</a><script data-card-contents-for-user="649778" type="text/json">{"id":649778,"first_name":"Richard","last_name":"Madgwick","domain_name":"cardiff","page_name":"RichardMadgwick","display_name":"Richard Madgwick","profile_url":"https://cardiff.academia.edu/RichardMadgwick?f_ri=409","photo":"https://0.academia-photos.com/649778/224538/262676/s65_richard.madgwick.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-37506926">+1</span><div class="hidden js-additional-users-37506926"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/IestynJones">Iestyn Jones</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-37506926'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-37506926').html(); 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Early medieval enclosure at Glanfred, near Llandre, Ceredigion. Archaeologia Cambrensis 167: 221-243. \n\nGeophysical survey and small-scale trial excavations were carried out on a small parchmark enclosure at Glanfred, near Llandre, Ceredigion in 2013. Geophysical survey revealed sections of the enclosure ditch that had not been previously visible from aerial photography, a number of possible entrances and two concentrations of internal anomalies. Excavation targeted a section of the inner of two ditches on the eastern side of the enclosure and an anomaly within the enclosure. An in situ iron slag deposit was discovered with an associated context dated between the late seventh and ninth century AD, whilst charred oats discovered in one of the lower deposits within the ditch was dated between the mid-fifth to sixth centuries AD. 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work_68584554" data-work_id="68584554" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/68584554/The_processing_of_hexagonally_sampled_signals_with_standard_rectangular_techniques_Application_to_2_D_large_aperture_synthesis_interferometric_radiometers">The processing of hexagonally sampled signals with standard rectangular techniques: Application to 2-D large aperture synthesis interferometric radiometers</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">AbstractIn Earth observation programs there is a need of passive low frequency (L-band) measurements to monitor soil moisture and ocean salinity with high spatial resolution 1020 Km, a radiometric resolution of 1K and a revisit time of... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_68584554" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">AbstractIn Earth observation programs there is a need of passive low frequency (L-band) measurements to monitor soil moisture and ocean salinity with high spatial resolution 1020 Km, a radiometric resolution of 1K and a revisit time of 13 days [1]. Compared to total power radiometers ...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/68584554" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="0e603b73e4a57889d5780860636858e2" rel="nofollow" data-download="{"attachment_id":79012049,"asset_id":68584554,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/79012049/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="97603630" href="https://upc.academia.edu/FrancescTorres">Francesc Torres</a><script data-card-contents-for-user="97603630" type="text/json">{"id":97603630,"first_name":"Francesc","last_name":"Torres","domain_name":"upc","page_name":"FrancescTorres","display_name":"Francesc Torres","profile_url":"https://upc.academia.edu/FrancescTorres?f_ri=409","photo":"https://0.academia-photos.com/97603630/95860357/84964829/s65_francesc.torres.png"}</script></span></span></li><li class="js-paper-rank-work_68584554 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="68584554"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 68584554, container: ".js-paper-rank-work_68584554", }); 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All sites are dated based on archaeological information and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_69086642" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Three kilns and a collection of baked bricks from Italian archaeological sites have been studied for archaeointensity determination using the Thellier method as modified by Coe. All sites are dated based on archaeological information and their ages range from 500 to 800 AD and 1500 to 1700 AD. Rock magnetic studies identify magnetite, Ti- magnetite and hematite as the main magnetic minerals, and magnetic susceptibility versus temperature shows a good thermal stability of the samples. The intensity results have been corrected for anisotropy of the thermoremanent magnetization and cooling rate effects. The new data together with 136 previously published results are used to estimate the variation of the Earth&#39;s magnetic field over the past three millennia. The time distribution of the Italian absolute intensity data is irregular with the majority of determinations concentrated during the last four centuries, while older periods are very poorly covered. Most of the data come from vo...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/69086642" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="ac1bcd9df7ca0d8d6411ac087c9d788e" rel="nofollow" data-download="{"attachment_id":79319687,"asset_id":69086642,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/79319687/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="54784664" href="https://independent.academia.edu/CampsPierre">Pierre Camps</a><script data-card-contents-for-user="54784664" type="text/json">{"id":54784664,"first_name":"Pierre","last_name":"Camps","domain_name":"independent","page_name":"CampsPierre","display_name":"Pierre Camps","profile_url":"https://independent.academia.edu/CampsPierre?f_ri=409","photo":"https://0.academia-photos.com/54784664/18199492/18180730/s65_pierre.camps.png"}</script></span></span></li><li class="js-paper-rank-work_69086642 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="69086642"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 69086642, container: ".js-paper-rank-work_69086642", }); 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$(".js-view-count[data-work-id=69086642]").text(description); $(".js-view-count-work_69086642").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_69086642").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="69086642"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">14</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="409" href="https://www.academia.edu/Documents/in/Geophysics">Geophysics</a>, <script data-card-contents-for-ri="409" type="text/json">{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="7475" href="https://www.academia.edu/Documents/in/Rock_magnetism">Rock magnetism</a>, <script data-card-contents-for-ri="7475" type="text/json">{"id":7475,"name":"Rock magnetism","url":"https://www.academia.edu/Documents/in/Rock_magnetism?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="32310" href="https://www.academia.edu/Documents/in/Archaeomagnetism">Archaeomagnetism</a><script data-card-contents-for-ri="32310" type="text/json">{"id":32310,"name":"Archaeomagnetism","url":"https://www.academia.edu/Documents/in/Archaeomagnetism?f_ri=409","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=69086642]'), work: {"id":69086642,"title":"Archaeointensity determinations from Italy: new data and the Earth's magnetic field strength variation over the past three millennia","created_at":"2022-01-21T21:27:57.182-08:00","url":"https://www.academia.edu/69086642/Archaeointensity_determinations_from_Italy_new_data_and_the_Earths_magnetic_field_strength_variation_over_the_past_three_millennia?f_ri=409","dom_id":"work_69086642","summary":"Three kilns and a collection of baked bricks from Italian archaeological sites have been studied for archaeointensity determination using the Thellier method as modified by Coe. All sites are dated based on archaeological information and their ages range from 500 to 800 AD and 1500 to 1700 AD. Rock magnetic studies identify magnetite, Ti- magnetite and hematite as the main magnetic minerals, and magnetic susceptibility versus temperature shows a good thermal stability of the samples. The intensity results have been corrected for anisotropy of the thermoremanent magnetization and cooling rate effects. The new data together with 136 previously published results are used to estimate the variation of the Earth\u0026#39;s magnetic field over the past three millennia. The time distribution of the Italian absolute intensity data is irregular with the majority of determinations concentrated during the last four centuries, while older periods are very poorly covered. Most of the data come from vo...","downloadable_attachments":[{"id":79319687,"asset_id":69086642,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":54784664,"first_name":"Pierre","last_name":"Camps","domain_name":"independent","page_name":"CampsPierre","display_name":"Pierre Camps","profile_url":"https://independent.academia.edu/CampsPierre?f_ri=409","photo":"https://0.academia-photos.com/54784664/18199492/18180730/s65_pierre.camps.png"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=409","nofollow":false},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false},{"id":7475,"name":"Rock magnetism","url":"https://www.academia.edu/Documents/in/Rock_magnetism?f_ri=409","nofollow":false},{"id":32310,"name":"Archaeomagnetism","url":"https://www.academia.edu/Documents/in/Archaeomagnetism?f_ri=409","nofollow":false},{"id":34754,"name":"Magnetic field","url":"https://www.academia.edu/Documents/in/Magnetic_field?f_ri=409"},{"id":143986,"name":"Archeomagnetism","url":"https://www.academia.edu/Documents/in/Archeomagnetism?f_ri=409"},{"id":147636,"name":"Cooling Rate","url":"https://www.academia.edu/Documents/in/Cooling_Rate?f_ri=409"},{"id":149117,"name":"Magnetic Susceptibility","url":"https://www.academia.edu/Documents/in/Magnetic_Susceptibility?f_ri=409"},{"id":162010,"name":"Geomatic Engineering","url":"https://www.academia.edu/Documents/in/Geomatic_Engineering?f_ri=409"},{"id":389180,"name":"Thermal Stability","url":"https://www.academia.edu/Documents/in/Thermal_Stability?f_ri=409"},{"id":411513,"name":"Geophysical","url":"https://www.academia.edu/Documents/in/Geophysical?f_ri=409"},{"id":688910,"name":"Volcanic Rock","url":"https://www.academia.edu/Documents/in/Volcanic_Rock?f_ri=409"},{"id":999570,"name":"Secular Variation","url":"https://www.academia.edu/Documents/in/Secular_Variation?f_ri=409"},{"id":1002225,"name":"Directional Data","url":"https://www.academia.edu/Documents/in/Directional_Data?f_ri=409"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_75176712" data-work_id="75176712" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/75176712/Meteorological_tsunamis_on_the_coasts_of_British_Columbia_and_Washington">Meteorological tsunamis on the coasts of British Columbia and Washington</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/75176712" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="9e0e4abfb68c211f9b9e223a24ab1bec" rel="nofollow" data-download="{"attachment_id":83051486,"asset_id":75176712,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/83051486/download_file?st=MTczMjQ1Mjc3OSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="115922819" href="https://independent.academia.edu/RabinovichAlexander">Alexander Rabinovich</a><script data-card-contents-for-user="115922819" type="text/json">{"id":115922819,"first_name":"Alexander","last_name":"Rabinovich","domain_name":"independent","page_name":"RabinovichAlexander","display_name":"Alexander Rabinovich","profile_url":"https://independent.academia.edu/RabinovichAlexander?f_ri=409","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_75176712 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="75176712"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 75176712, container: ".js-paper-rank-work_75176712", }); 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$(".js-view-count[data-work-id=75176712]").text(description); $(".js-view-count-work_75176712").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_75176712").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="75176712"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">8</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="407" href="https://www.academia.edu/Documents/in/Geochemistry">Geochemistry</a>, <script data-card-contents-for-ri="407" type="text/json">{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="409" href="https://www.academia.edu/Documents/in/Geophysics">Geophysics</a>, <script data-card-contents-for-ri="409" type="text/json">{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="18625" href="https://www.academia.edu/Documents/in/Sea_Level">Sea Level</a><script data-card-contents-for-ri="18625" type="text/json">{"id":18625,"name":"Sea Level","url":"https://www.academia.edu/Documents/in/Sea_Level?f_ri=409","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=75176712]'), work: {"id":75176712,"title":"Meteorological tsunamis on the coasts of British Columbia and Washington","created_at":"2022-04-01T12:29:15.083-07:00","url":"https://www.academia.edu/75176712/Meteorological_tsunamis_on_the_coasts_of_British_Columbia_and_Washington?f_ri=409","dom_id":"work_75176712","summary":null,"downloadable_attachments":[{"id":83051486,"asset_id":75176712,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":115922819,"first_name":"Alexander","last_name":"Rabinovich","domain_name":"independent","page_name":"RabinovichAlexander","display_name":"Alexander Rabinovich","profile_url":"https://independent.academia.edu/RabinovichAlexander?f_ri=409","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=409","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=409","nofollow":false},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false},{"id":18625,"name":"Sea Level","url":"https://www.academia.edu/Documents/in/Sea_Level?f_ri=409","nofollow":false},{"id":148176,"name":"Atmospheric Pressure","url":"https://www.academia.edu/Documents/in/Atmospheric_Pressure?f_ri=409"},{"id":174781,"name":"Oscillations","url":"https://www.academia.edu/Documents/in/Oscillations?f_ri=409"},{"id":198379,"name":"British Columbia","url":"https://www.academia.edu/Documents/in/British_Columbia?f_ri=409"},{"id":447469,"name":"Washington State","url":"https://www.academia.edu/Documents/in/Washington_State?f_ri=409"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_64843223 coauthored" data-work_id="64843223" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/64843223/Growing_strong_and_growing_fast_The_SEG_Womens_Network">Growing strong and growing fast: The SEG Women's Network</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The SEG Women&#39;s Network invites you to attend its Networking Breakfast at the upcoming SEG Annual Meeting in Denver, Colorado, at 8:30 to 11:00 a.m. on 29 October. This year, the program will enlist four panelists: Sally Zinke, SEG... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_64843223" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The SEG Women&#39;s Network invites you to attend its Networking Breakfast at the upcoming SEG Annual Meeting in Denver, Colorado, at 8:30 to 11:00 a.m. on 29 October. This year, the program will enlist four panelists: Sally Zinke, SEG President, 2000; Allison Malcolm, SEG Clarence Karcher Award winner, 2012; Louise Pellerin, SEG Life Membership Award winner, 2014; and Sue Webb, SEG Outstanding Educator Award winner, 2014. They will describe their own journeys of success before opening the floor to a facilitated discussion with questions from the audience.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/64843223" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="40978116" href="https://independent.academia.edu/CapelloMariaAngela">Maria Angela Capello</a><script data-card-contents-for-user="40978116" type="text/json">{"id":40978116,"first_name":"Maria Angela","last_name":"Capello","domain_name":"independent","page_name":"CapelloMariaAngela","display_name":"Maria Angela Capello","profile_url":"https://independent.academia.edu/CapelloMariaAngela?f_ri=409","photo":"/images/s65_no_pic.png"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-64843223">+1</span><div class="hidden js-additional-users-64843223"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/ESprunt">Eve Sprunt</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-64843223'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-64843223').html(); } } new HoverPopover(popoverSettings); })();</script></li><li class="js-paper-rank-work_64843223 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="64843223"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 64843223, container: ".js-paper-rank-work_64843223", }); });</script></li><li class="js-percentile-work_64843223 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 64843223; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_64843223"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_64843223 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="64843223"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 64843223; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=64843223]").text(description); $(".js-view-count-work_64843223").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_64843223").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="64843223"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">2</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="184" href="https://www.academia.edu/Documents/in/Sociology">Sociology</a>, <script data-card-contents-for-ri="184" type="text/json">{"id":184,"name":"Sociology","url":"https://www.academia.edu/Documents/in/Sociology?f_ri=409","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="409" href="https://www.academia.edu/Documents/in/Geophysics">Geophysics</a><script data-card-contents-for-ri="409" type="text/json">{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=64843223]'), work: {"id":64843223,"title":"Growing strong and growing fast: The SEG Women's Network","created_at":"2021-12-17T07:13:02.999-08:00","url":"https://www.academia.edu/64843223/Growing_strong_and_growing_fast_The_SEG_Womens_Network?f_ri=409","dom_id":"work_64843223","summary":"The SEG Women\u0026#39;s Network invites you to attend its Networking Breakfast at the upcoming SEG Annual Meeting in Denver, Colorado, at 8:30 to 11:00 a.m. on 29 October. This year, the program will enlist four panelists: Sally Zinke, SEG President, 2000; Allison Malcolm, SEG Clarence Karcher Award winner, 2012; Louise Pellerin, SEG Life Membership Award winner, 2014; and Sue Webb, SEG Outstanding Educator Award winner, 2014. They will describe their own journeys of success before opening the floor to a facilitated discussion with questions from the audience.","downloadable_attachments":[],"ordered_authors":[{"id":40978116,"first_name":"Maria Angela","last_name":"Capello","domain_name":"independent","page_name":"CapelloMariaAngela","display_name":"Maria Angela Capello","profile_url":"https://independent.academia.edu/CapelloMariaAngela?f_ri=409","photo":"/images/s65_no_pic.png"},{"id":62606815,"first_name":"Eve","last_name":"Sprunt","domain_name":"independent","page_name":"ESprunt","display_name":"Eve Sprunt","profile_url":"https://independent.academia.edu/ESprunt?f_ri=409","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":184,"name":"Sociology","url":"https://www.academia.edu/Documents/in/Sociology?f_ri=409","nofollow":false},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=409","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div></div><div class="u-taCenter Pagination"><ul class="pagination"><li class="next_page"><a href="/Documents/in/Geophysics?after=50%2C64843223" rel="next">Next</a></li><li class="last next"><a href="/Documents/in/Geophysics?page=last">Last »</a></li></ul></div></div><div class="hidden-xs hidden-sm"><div class="u-pl6x"><div style="width: 300px;"><div class="panel panel-flat u-mt7x"><div class="panel-heading u-p5x"><div class="u-tcGrayDark u-taCenter u-fw700 u-textUppercase">Related Topics</div></div><ul class="list-group"><li class="list-group-item media_v2 u-mt0x u-p3x"><div class="media-body"><div class="u-tcGrayDarker u-fw700"><a class="u-tcGrayDarker" href="https://www.academia.edu/Documents/in/Geology">Geology</a></div></div><div class="media-right media-middle"><a class="u-tcGreen u-textDecorationNone u-linkUnstyled u-fw500 hidden" data-follow-ri-id="406">Follow</a><a class="u-tcGray u-textDecorationNone u-linkUnstyled u-fw500 hidden" 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