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Evidence for Pliocene–Quaternary normal faulting in the hinterland of the Bhutan Himalaya
Evidence for Pliocene–Quaternary normal faulting in the hinterland of the Bhutan Himalaya Abstract In the central Himalaya, past researchers have identified a distinctive transition from the physiogra...
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Sign In Chalcedony vein horizons and clastic dikes in the White River Group as products of diagenetically driven deformation ↵*E-mail: harmon_maher{at}mail.unomaha.edu. ...
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Web host: | Microsoft Corporation |
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Updated: | October 06, 2023 |
Expires: | September 24, 2024 |
Created: | September 24, 2008 |
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