Biomarker and Carbon Isotopic Evidence of Marine Incursions in the Himalayan Foreland Basin During Its Overfilled Stage
Author:
Affiliation:
1. Department of Earth Sciences Indian Institute of Science Education and Research Kolkata Mohanpur India
2. Centre for Climate and Environmental Studies Indian Institute of Science Education and Research Kolkata Mohanpur India
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Atmospheric Science,Oceanography
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020PA004083
Reference199 articles.
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2. Evolution of the Himalayan Paleogene foreland basin, influence of its litho-packet on the formation of thrust-related domes and windows in the Eastern Himalayas – A review
3. Siwalik stratigraphy and its bearing on the main boundary fault;Acharyya S. K.;Geological Survey of India,1979
4. Earliest Miocene planktonic foraminifera from Kalijhora area, Tista river section, Darjeeling Sub‐Himalaya;Acharyya S. K.;Indian Minerals,1987
5. Geochemical characterisation of Fika Formation in the Chad (Bornu) Basin, northeastern Nigeria: Implications for depositional environment and tectonic setting
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