Microstructure and geochemistry of pseudotachylyte veins from Sarwar‐Junia Fault Zone, India: Implications for frictional melting process in a seismic fault zone
Author:
Affiliation:
1. Department of Geology University of Delhi Delhi India
Funder
University Grants Commission
University of Delhi
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3900
Reference94 articles.
1. Adhikari S. &Pyne T. K.(1981).A report on the systematic geological mapping in parts of Tonk and Ajmer districts Rajasthan (Unpublished report Geological Survey of India Calcutta).
2. Mechanism of frictional fusion in fault zones
3. A multi-kilometer pseudotachylyte system as an exhumed record of earthquake rupture geometry at hypocentral depths (Colorado, USA)
4. Structural geometry and thermal history of pseudotachylyte from the Homestake Shear Zone, Sawatch Range, Colorado;Allen J. L.;Field Guides,2002
5. Phase equilibria modeling in igneous petrology: use of COMAGMAT model for simulating fractionation of ferro-basaltic magmas and the genesis of high-alumina basalt
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1. Pseudotachylytes in felsic lower-crustal rocks of the Calabrian Serre massif: A record of deep- or shallow-crustal earthquakes?;Lithos;2023-12
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3. U–Pb geochronology and metamorphic history of gneissic rocks from Sarwar‐Junia Fault Zone, Rajasthan, NW India: Implications for the tectonothermal evolution of the Aravalli‐Delhi Mobile Belt;Geological Journal;2023-08-29
4. Features of Frictional Melting of Rocks and Melt Crystallization in a Seismic Process: Case Study of Pseudotachylites of the Ladoga Region;Izvestiya, Physics of the Solid Earth;2022-12
5. Strength enhanced by pseudotachylite melt in fault zone rocks during post-seismic melting: A case study from the Gangavalli fault zone, southern India;Journal of Earth System Science;2022-09-24
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