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Abstract: How does the chemico-mineralogical transition in fluid-mediated faults explain recurrences of low-to-moderate magnitude seismic tremors? - A case study from the Koyna-Warna Intraplate Region, Western India. (AGU25)

How does the chemico-mineralogical transition in fluid-mediated faults explain recurrences of low-to-moderate magnitude seismic tremors? - A case study from the Koyna-Warna Intraplate Region, Western India.

Piyal Halder1,2 and Anupam Sharma1,2, (1)Academy of Scientific and Innovative Research (AcSIR), Ghaziabad, India, (2)Birbal Sahni Institute of Palaeosciences (DST, Govt. of India), Lucknow, India