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2019 | OriginalPaper | Chapter

NE-SW Strike-Slip Fault in the Granitoid from the Margin of the South East Dharwar Craton, Degloor, Nanded District, Maharashtra, India

Authors : Md. Babar, R. D. Kaplay, Soumyajit Mukherjee, Souradeep Mahato, Chandrakant Gurav

Published in: Tectonics and Structural Geology: Indian Context

Publisher: Springer International Publishing

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Abstract

The E-W strike-slip brittle faults are reported from the margin of South East Deccan Volcanic Province (SEDVP) near Kinwat where we detail faulting, folding and boudinaging from the Adampur-Bhaisa profile along the SEDVP margin further SW of the Kinwat region. The present study focusses deformations in the basement granite from the SEDVP around Degloor/Diglur. The NE trending strike-slip faults, W-dipping steep normal faults, and W verging thrusts are documented in this study in the granitic rocks. NE trending strike-slip tectonics dominates the study area, which does not corroborate with ~E trending Western Boundary East Dharwar Craton Strike-Slip Zone (WBEDCSZ). The concentrated strike-slip deformation at Degloor lies between (micro)seismically active Killari-Nanded-Kaddam regions. The present study suggests that the stretch of >75 km, from Degloor to Bhaisa, along the SEDVP margin within the EDC, is a tectonic zone and is designated as Western Boundary East Dharwar Craton Deformed Zone (WBEDCDZ). Difference in trends of stress axes (e.g., the least principal stress axis σ3 ranging 20–83°N) deciphered mainly from conjugate joints shows local-scale heterogeneity in the stress regime.

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Metadata
Title
NE-SW Strike-Slip Fault in the Granitoid from the Margin of the South East Dharwar Craton, Degloor, Nanded District, Maharashtra, India
Authors
Md. Babar
R. D. Kaplay
Soumyajit Mukherjee
Souradeep Mahato
Chandrakant Gurav
Copyright Year
2019
DOI
https://doi.org/10.1007/978-3-319-99341-6_5