Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/8897
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dc.contributor.advisorTRIPATHY, GYANA RANJAN-
dc.contributor.authorSAMAL, SANKET-
dc.date.accessioned2024-05-20T10:59:41Z-
dc.date.available2024-05-20T10:59:41Z-
dc.date.issued2024-05-
dc.identifier.citation35en_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/8897-
dc.description.abstractThe Panjal Trap represents one of the largest outcrops of early Permian Period (~290Ma) volcanism associated with the separation of Cimmeria from Gondwana and opening of the Neothethys Ocean. In the Indian sector, these rocks are exposed in the Northern Himalayas along the Pir Panjal and Zanskar mountain ranges. While existing studies have provided detailed geological understanding of these volcanisms, few studies examine the geochemical variations associated with them. This thesis undertakes a geochemical study of the Panjal Traps from the less explored south-eastern Zanskar region to investigate regional variations in composition, petrogenesis and tectonics.en_US
dc.description.sponsorshipIISER Puneen_US
dc.language.isoenen_US
dc.subjectGeochemistryen_US
dc.subjectIgneous Petrologyen_US
dc.subjectPanjal Trapsen_US
dc.subjectBasaltsen_US
dc.subjectE-MORBen_US
dc.titleGeochemistry of Panjal Traps from Zanskar Region: Implications for petrogenesis and geochemical variabilitiesen_US
dc.typeThesisen_US
dc.description.embargoTwo Yearsen_US
dc.type.degreeMSc.en_US
dc.contributor.departmentDept. of Earth and Climate Scienceen_US
dc.contributor.registration20226401en_US
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