Mineralogical and Geochemical Evidence of Fluid‐rock Interaction at the Shallow Crustal Level in Koyna Seismogenic Region, Maharashtra, India: Impact and Implications-Reference-Cited by-同舟云学术

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Mineralogical and Geochemical Evidence of Fluid‐rock Interaction at the Shallow Crustal Level in Koyna Seismogenic Region, Maharashtra, India: Impact and Implications

Published:2021-11 Issue:S1 Volume:95 Page:40-43
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica (Eng)

Author:

PIYAL Halder¹,MATSYENDRA Kumar Shukla²,KAMLESH Kumar¹,ANUPAM Sharma¹

Affiliation:

1. Birbal Sahni Institute of Palaeosciences (DST, Govt. of India) Lucknow U.P. India

2. Govt. of India, Ministry of Earth Sciences Borehole Geophysics Research Laboratory, Karad Maharashtra India

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14827

Reference19 articles.

1. Geophysical anomalies over epithermal systems

2. Smectite dehydration–its relation to structural development and hydrocarbon accumulation in Northern Gulf of Mexico basin;Bruce C.H.;AAPG Bulletin,1985

3. Fault zone fabric and fault weakness

4. Glassley E.W. Crossey J.L. andMontanez P.I. 2016.Fluid-rock interaction. Encyclopedia of Geochemistry.https://doi.org/10.1007/978-3-319-39193-9_36-1.

5. Delineation of Damage Zones From 3 km Downhole Geophysical Logs in the Koyna Seismogenic Zone, Western India

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Fluid–rock interaction in the basement granitoids: A plausible answer to recurring seismicity;Journal of Palaeosciences;2023-07-14

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