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[India | IJRASET Publication - Academia.edu</title> <link rel="canonical" href="https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India" /> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "single_work", 'action': "show", 'controller_action': 'single_work#show', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script> var $controller_name = 'single_work'; var $action_name = "show"; var $rails_env = 'production'; var $app_rev = '81343a4e95ee3e0047e8d2b44f059f00b3d8f087'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.require = { config: function() { return function() {} } } </script> <script> window.Aedu = window.Aedu || {}; window.Aedu.hit_data = null; window.Aedu.serverRenderTime = new Date(1733341068000); window.Aedu.timeDifference = new Date().getTime() - 1733341068000; </script> <script type="application/ld+json">{"@context":"https://schema.org","@type":"ScholarlyArticle","abstract":"The petrography and mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy. The petrographic and mineralogical studies also play an important role identification of various petrogenetic processes that may be responsible for producing them. In the present study an attempt has been made to understand the preliminary petrography and mineralogy of lava pile of Muktagiri. The detailed geological mapping of the study area was done, and number of filed traverses were carried out the to identify the various lava flows along with their extensions. The field specimens were collected along all the traverses. The megascopic and microscopic studies were done to identify the petrographic and mineralogical characters. About 15 lava flows were identified in the study area. These lava flows, based on mineralogical and petrographic characters were divided in to four formations namely A, B, C and D formation. Further, the lava flows can be classified into aphyric and phyric lava flows. Mineralogical study revels that the lava flows are composed of plagioclase, clinopyroxene and opaque (mostly Fe-Ti oxide). At few places places primary glass with very small proportion of olivine is also observed.","author":[{"@context":"https://schema.org","@type":"Person","name":"IJRASET Publication"}],"contributor":[],"dateCreated":"2021-02-24","dateModified":"2021-02-24","datePublished":"2021-01-01","headline":"Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India","identifier":{"@type":"PropertyValue","propertyID":"DOI","value":"10.22214/ijraset.2021.32923"},"image":"https://attachments.academia-assets.com/65767064/thumbnails/1.jpg","inLanguage":"en","keywords":["Mineralogy","Petrography","Lava Flows","Deccan Basalts","Muktagiri"],"publication":"International Journal for Research in Applied Science \u0026 Engineering Technology","publisher":{"@context":"https://schema.org","@type":"Organization","name":null},"sameAs":"https://doi.org/10.22214/ijraset.2021.32923","sourceOrganization":[{"@context":"https://schema.org","@type":"EducationalOrganization","name":null}],"thumbnailUrl":"https://attachments.academia-assets.com/65767064/thumbnails/1.jpg","url":"https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India"}</script><link rel="stylesheet" media="all" 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mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy. The petrographic and mineralogical studies also play an important role identification of various petrogenetic processes that may be responsible for producing them. In the present study an attempt has been made to understand the preliminary petrography and mineralogy of lava pile of Muktagiri. The detailed geological mapping of the study area was done, and number of filed traverses were carried out the to identify the various lava flows along with their extensions. The field specimens were collected along all the traverses. The megascopic and microscopic studies were done to identify the petrographic and mineralogical characters. About 15 lava flows were identified in the study area. These lava flows, based on mineralogical and petrographic characters were divided in to four formations namely A, B, C and D formation. Further, the lava flows can be classified into aphyric and phyric lava flows. Mineralogical study revels that the lava flows are composed of plagioclase, clinopyroxene and opaque (mostly Fe-Ti oxide). At few places places primary glass with very small proportion of olivine is also observed.","publication_date":"2021,,","publication_name":"International Journal for Research in Applied Science \u0026 Engineering Technology"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India","broadcastable":true,"draft":false,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [6079060]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "control"; window.loswp.useOptimizedScribd4genScript = false; window.loswp.appleClientId = 'edu.academia.applesignon';</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div class="ds-work-card--grid-container"><div class="ds-work-card--container js-loswp-work-card"><div class="ds-work-card--cover"><div class="ds-work-cover--wrapper"><div class="ds-work-cover--container"><button class="ds-work-cover--clickable js-swp-download-button" data-signup-modal="{"location":"swp-splash-paper-cover","attachmentId":65767064,"attachmentType":"pdf"}"><img alt="First page of “Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India”" class="ds-work-cover--cover-thumbnail" src="https://0.academia-photos.com/attachment_thumbnails/65767064/mini_magick20210224-14621-1dihjmv.png?1614165972" /><img alt="PDF Icon" class="ds-work-cover--file-icon" src="//a.academia-assets.com/assets/single_work_splash/adobe.icon-574afd46eb6b03a77a153a647fb47e30546f9215c0ee6a25df597a779717f9ef.svg" /><div class="ds-work-cover--hover-container"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span><p>Download Free PDF</p></div><div class="ds-work-cover--ribbon-container">Download Free PDF</div><div class="ds-work-cover--ribbon-triangle"></div></button></div></div></div><div class="ds-work-card--work-information"><h1 class="ds-work-card--work-title">Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India</h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="6079060" href="https://independent.academia.edu/IJRASETPublication"><img alt="Profile image of IJRASET Publication" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/6079060/2549300/33111525/s65_ijraset.publication.jpg" />IJRASET Publication</a></div><div class="ds-work-card--detail"><p class="ds-work-card--detail ds2-5-body-sm">2021, International Journal for Research in Applied Science & Engineering Technology</p><a class="js-loswp-work-card-doi-link ds2-5-body-sm ds2-5-body-link" href="https://doi.org/10.22214/ijraset.2021.32923" rel="nofollow">https://doi.org/10.22214/ijraset.2021.32923</a><div class="ds-work-card--work-metadata"><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">visibility</span><p class="ds2-5-body-sm" id="work-metadata-view-count">…</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">description</span><p class="ds2-5-body-sm">8 pages</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">link</span><p class="ds2-5-body-sm">1 file</p></div></div><script>(async () => { const workId = 45181234; const worksViewsPath = "/v0/works/views?subdomain_param=api&work_ids%5B%5D=45181234"; const getWorkViews = async (workId) => { const response = await fetch(worksViewsPath); if (!response.ok) { throw new Error('Failed to load work views'); } const data = await response.json(); return data.views[workId]; }; // Get the view count for the work - we send this immediately rather than waiting for // the DOM to load, so it can be available as soon as possible (but without holding up // the backend or other resource requests, because it's a bit expensive and not critical). const viewCount = await getWorkViews(workId); const updateViewCount = (viewCount) => { const viewCountNumber = Number(viewCount); if (!viewCountNumber) { throw new Error('Failed to parse view count'); } const commaizedViewCount = viewCountNumber.toLocaleString(); const viewCountBody = document.getElementById('work-metadata-view-count'); if (viewCountBody) { viewCountBody.textContent = `${commaizedViewCount} views`; } else { throw new Error('Failed to find work views element'); } }; // If the DOM is still loading, wait for it to be ready before updating the view count. if (document.readyState === "loading") { document.addEventListener('DOMContentLoaded', () => { updateViewCount(viewCount); }); // Otherwise, just update it immediately. } else { updateViewCount(viewCount); } })();</script></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">The petrography and mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy. The petrographic and mineralogical studies also play an important role identification of various petrogenetic processes that may be responsible for producing them. In the present study an attempt has been made to understand the preliminary petrography and mineralogy of lava pile of Muktagiri. The detailed geological mapping of the study area was done, and number of filed traverses were carried out the to identify the various lava flows along with their extensions. The field specimens were collected along all the traverses. The megascopic and microscopic studies were done to identify the petrographic and mineralogical characters. About 15 lava flows were identified in the study area. These lava flows, based on mineralogical and petrographic characters were divided in to four formations namely A, B, C and D formation. Further, the lava flows can be classified into aphyric and phyric lava flows. Mineralogical study revels that the lava flows are composed of plagioclase, clinopyroxene and opaque (mostly Fe-Ti oxide). At few places places primary glass with very small proportion of olivine is also observed.</p><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--work-card","attachmentId":65767064,"attachmentType":"pdf","workUrl":"https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India"}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--work-card","attachmentId":65767064,"attachmentType":"pdf","workUrl":"https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India"}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div></div><div data-auto_select="false" 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class="ds-related-work--abstract ds2-5-body-sm">Deccan Traps are made up of basaltic lava flows of Upper Cretaceous to Lower Eocene age. These flows have been formed by fissure type of volcanoes. They form a part of plateau basalts of the Peninsular India. The flows are of 'aa' type. The study area Tumjai Hill falls in Kumbhi River Basin. The altitude ranges from 539 meters to 889 meters. The total thickness of Tumjai Hill lava flows is 350 meters. The lava flow mapping has been carried out in the study area and various flows are marked. There are seven lava flows in Tumjai Hill area. Each flow is composed of several sub units. The sub units are made up of jointed basalt, compact basalt, vesicular and amygdaloidal basalt, red bole and volcanic breccia. Rosette structure and spheroidal weathering are also seen. Columnar joints are present in the upper part of the hill. The volcanic breccia is formed at the top of the lava flows at some places. In which the angular rock fragments are mingled with lava. The patches of red bole mark the boundary of the successive lava flows at many places. The compact basalt is generally devoid of vesicles. In the study area the compact columnar jointing is found restricted to only some parts of the lava flows. In the study area the commonly observed feature of the flows is spheroidal weathering. The general trend of the flows is horizontal.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Lithostratigraphy of Lava Flows at Tumjai Hill, Kolhapur District, Maharashtra, India","attachmentId":65669068,"attachmentType":"pdf","work_url":"https://www.academia.edu/45104669/Lithostratigraphy_of_Lava_Flows_at_Tumjai_Hill_Kolhapur_District_Maharashtra_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/45104669/Lithostratigraphy_of_Lava_Flows_at_Tumjai_Hill_Kolhapur_District_Maharashtra_India"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="9113476" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/9113476/Petrographic_Study_of_the_Magmatic_body_of_Bhanjada_Bet_Gujarat">Petrographic Study of the Magmatic body of Bhanjada Bet, Gujarat</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="7102400" href="https://presiuniv.academia.edu/KUHUCHAKRABORTY">KUHU CHAKRABORTY</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The magmatic bodies of Gujarat are well studied throughout th e years. But the rocks of the isolated magmatic body of Bhanjada Bet, are not largely studied. The present work aims to study the field occurence of the rocks, its petrography and the general tectonic setting of the formation of the rocks of the island. The main mass is largely composed of phonolite surrounded by nepheline-syenite at the periphery. From the modal analysis, the coarse grained rocks are named as foid-monzo syenite, while its volcanic equivalent as phonolite. the major minerals of both the rock types are alkali-feldspar, plagioclase-feldspar, nepheline, aegirine etc. The presence of these types of rocks indicated silica under-saturated melt composition. These rocks typicaly represents the continental rift setting, which is evident from the fact that Bhanjada Bet is a part of the Kutch rift.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Petrographic Study of the Magmatic body of Bhanjada Bet, Gujarat","attachmentId":35406010,"attachmentType":"pdf","work_url":"https://www.academia.edu/9113476/Petrographic_Study_of_the_Magmatic_body_of_Bhanjada_Bet_Gujarat","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/9113476/Petrographic_Study_of_the_Magmatic_body_of_Bhanjada_Bet_Gujarat"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="12912402" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/12912402/PETROGRAPHY_AND_GEOCHEMISTRY_OF_MAFIC_ROCKS_IN_AND_AROUND_SATI_AND_SARASPADA_NORTH_OF_BISOI_MAYURBHANJ_DISTRICT_NORTHERN_PART_OF_STATE_ORISSA_EASTERN_INDIA">PETROGRAPHY AND GEOCHEMISTRY OF MAFIC ROCKS IN AND AROUND SATI AND SARASPADA, NORTH OF BISOI, MAYURBHANJ DISTRICT, NORTHERN PART OF STATE ORISSA, EASTERN INDIA</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="31900147" href="https://du-in.academia.edu/KALYANBRATAHATUI">KALYANBRATA HATUI</a></div><p class="ds-related-work--abstract ds2-5-body-sm">This Geological study has been carried out in and around Saraspada and Sati, Northern part of Bisoi in the Mayurbhanj district at the northern part of the state of Orissa. The principle objective of this study was to thoroughly study the mafic rocks of the area. Numerous outcrops of this type of rocks were observed in the study area. Various field measurements including trend, grain size, mutual distribution, association with granitic country rock and sampling were performed, which fall within the toposheet no: 73 J/8. The mesoarchean-Paleoproterozoic stratigraphic record of the Singbhum crustal province, eastern India, implies sedimentation and volcanism in a changing tectonic scenario and thus assumes geological significance. Mafic magmatism in the craton spreads from 3.3 Ga (Oldest enclaves of amphibolltes) to about 0.1 Ga (Newer dolerite dyke group). The present study is based on evolution of magmatic rocks in relation to tectonic setting in a region which is southern extension of Singbhum shear zone.These outcrops occur as chain of hillocks with low elevation. Trend wise they vary from two main orientations: NW-SE and NE-SW. The dykes show variable grain size, texture and mineralogy. These basic dykes are found exclusively associated with Singhbhum granite. The bodies range in width from 20m to over 60m and in length of around 100m. Grain size varies from medium to coarse, with some fine grained varieties restricted to contact zones. Mineralogically, the mafic rock is mainly composed of orthopyroxene, clinopyroxene and plagioclase feldspar. Clinopyroxene grains are most abundant. Orthopyroxene grains are stubby shaped and highly fractured. Solely consisted groundmass plagioclase grains are unusually large and trap the pyroxenes as inclusion. A true magmatic texture of minerals is observed. Alteration of mineral is found generally near the contact of granitic body, otherwise the rock is fresh. This work consists of detailed petrographic study with the aid of high power microscopes, geochemical analysis and plotting modal analysis data, major element compositions, normative calculations, AFM diagram along with variation diagrams. In this purpose three important parameters are used i.e. SiO2 content, Mg no. and Differential Index (D.I). From the plotting of modal analysis data the name of the rock is Mela-gabbronorite. High Mg no. indicates the primitive character of magma. Plotting of the samples in AFM diagram inferred iron enrichment trends of the magma.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"PETROGRAPHY AND GEOCHEMISTRY OF MAFIC ROCKS IN AND AROUND SATI AND SARASPADA, NORTH OF BISOI, MAYURBHANJ DISTRICT, NORTHERN PART OF STATE ORISSA, EASTERN INDIA","attachmentId":42789785,"attachmentType":"pdf","work_url":"https://www.academia.edu/12912402/PETROGRAPHY_AND_GEOCHEMISTRY_OF_MAFIC_ROCKS_IN_AND_AROUND_SATI_AND_SARASPADA_NORTH_OF_BISOI_MAYURBHANJ_DISTRICT_NORTHERN_PART_OF_STATE_ORISSA_EASTERN_INDIA","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/12912402/PETROGRAPHY_AND_GEOCHEMISTRY_OF_MAFIC_ROCKS_IN_AND_AROUND_SATI_AND_SARASPADA_NORTH_OF_BISOI_MAYURBHANJ_DISTRICT_NORTHERN_PART_OF_STATE_ORISSA_EASTERN_INDIA"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="55755848" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/55755848/Petrology_of_the_mafic_sill_of_Narshingpur_Lakhnadon_section_Eastern_Deccan_volcanic_province">Petrology of the mafic sill of Narshingpur-Lakhnadon section, Eastern Deccan volcanic province</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="29857308" href="https://independent.academia.edu/JyotisankarRay">Jyotisankar Ray</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of the Geological Society of India, 2011</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Petrology of the mafic sill of Narshingpur-Lakhnadon section, Eastern Deccan volcanic province","attachmentId":71476125,"attachmentType":"pdf","work_url":"https://www.academia.edu/55755848/Petrology_of_the_mafic_sill_of_Narshingpur_Lakhnadon_section_Eastern_Deccan_volcanic_province","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/55755848/Petrology_of_the_mafic_sill_of_Narshingpur_Lakhnadon_section_Eastern_Deccan_volcanic_province"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="114404625" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/114404625/Volcanology_and_lava_flow_morpho_types_from_the_Koyna_Warna_region_western_Deccan_Traps_India">Volcanology and lava flow morpho-types from the Koyna-Warna region, western Deccan Traps, India</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="20030334" href="https://unipune.academia.edu/RaymondDuraiswami">Raymond Duraiswami</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of the Geological Society of India, 2017</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Volcanology and lava flow morpho-types from the Koyna-Warna region, western Deccan Traps, India","attachmentId":111111566,"attachmentType":"pdf","work_url":"https://www.academia.edu/114404625/Volcanology_and_lava_flow_morpho_types_from_the_Koyna_Warna_region_western_Deccan_Traps_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/114404625/Volcanology_and_lava_flow_morpho_types_from_the_Koyna_Warna_region_western_Deccan_Traps_India"><span 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You can download the paper by clicking the button above.</p></div></div></div></div><div class="ds-sidebar--container js-work-sidebar"><div class="ds-related-content--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="0" data-entity-id="69899535" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/69899535/Geology_and_Petrogenesis_of_Igneous_Rocks_from_Batur_Paleovolcano_Gunungkidul_Yogyakarta_Evidence_from_their_Textures_Mineralogy_and_Major_Elements_Geochemistry">Geology and Petrogenesis of Igneous Rocks from Batur Paleovolcano, Gunungkidul, Yogyakarta: Evidence from their Textures, Mineralogy, and Major Elements Geochemistry</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="188413832" href="https://independent.academia.edu/AnastasiaTitisari">Anastasia Titisari</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of Applied Geology</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Geology and Petrogenesis of Igneous Rocks from Batur Paleovolcano, Gunungkidul, Yogyakarta: Evidence from their Textures, Mineralogy, and Major Elements Geochemistry","attachmentId":79819489,"attachmentType":"pdf","work_url":"https://www.academia.edu/69899535/Geology_and_Petrogenesis_of_Igneous_Rocks_from_Batur_Paleovolcano_Gunungkidul_Yogyakarta_Evidence_from_their_Textures_Mineralogy_and_Major_Elements_Geochemistry","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" href="https://www.academia.edu/69899535/Geology_and_Petrogenesis_of_Igneous_Rocks_from_Batur_Paleovolcano_Gunungkidul_Yogyakarta_Evidence_from_their_Textures_Mineralogy_and_Major_Elements_Geochemistry"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="1" data-entity-id="31008217" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/31008217/Flow_Mapping_and_Correlations_of_the_Deccan_Basalt_Lava_Flows_North_East_Maharashtra_India">Flow Mapping and Correlations of the Deccan Basalt Lava Flows, North-East Maharashtra, India</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="68700056" href="https://independent.academia.edu/ManishDeshmukh6">Dr. Manish S . 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href="https://www.academia.edu/30202270/Application_of_mineral_and_whole_rock_analysis_in_identification_of_petrogenesis_of_the_pillow_lavas_in_the_Nain_ophiolite">Application of mineral and whole rock analysis in identification of petrogenesis of the pillow lavas in the Nain ophiolite</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="4391121" href="https://modares.academia.edu/NargessShirdashtzadeh">Nargess Shirdashtzadeh</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2008</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Application of mineral and whole rock analysis in identification of petrogenesis of the pillow lavas in the Nain 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