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Please use this identifier to cite or link to this item: http://20.198.91.3:8080/jspui/handle/123456789/8511
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dc.contributor.advisorMondal, Tridib Kumar-
dc.contributor.authorShil, Barnali-
dc.date.accessioned2025-09-10T07:41:18Z-
dc.date.available2025-09-10T07:41:18Z-
dc.date.issued2019-
dc.date.submitted2019-
dc.identifier.otherDC4837-
dc.identifier.urihttp://20.198.91.3:8080/jspui/handle/123456789/8511-
dc.description.abstractIn this study, data from mesoscopic-scale brittle structures (faults) are used to decipher slip tendency analysis and relate it to regional-scale kinematics in granite (Mulgund, West Dharwar Craton, southern India) and it is done using Win Tensor software and it has been found that most of the vulnerable planes are oriented parallel to the compressive direction of D3 deformation.en_US
dc.format.extentvii, 35 p.en_US
dc.language.isoenen_US
dc.publisherJadavpur University, Kolkata, West Bengalen_US
dc.subjectSlip tendencyen_US
dc.subjectWin Tensoren_US
dc.titleSlip tendency analysis: implications on fault reactivationen_US
dc.typeTexten_US
dc.departmentJadavpur University, Dept. of Geological Sciencesen_US
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