Rock Magnetism of Late Cretaceous to Middle Eocene Strata in the Lesser Himalaya, Western Nepal: Inferences Regarding the Paleoenvironment

The growth of the southern piedmont of the Himalayan boundary and its depositional setting has changed since uplift of the Himalaya due to continental Indian-Eurasian collision, which has resulted in variation in magnetic minerals in marine- and terrestrial-facies sediments. In this paper, we utiliz...

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Principais autores:	Dhan Bahadur Khatri, Weilin Zhang, Xiaomin Fang, Qingquan Meng, Tao Zhang, Dawen Zhang, Khum N. Paudayal
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Frontiers Media S.A. 2021-10-01
coleção:	Frontiers in Earth Science
Assuntos:	rock magnetism Cretaceous to Eocene strata paleoenvironment transgression and regression Lesser Himalaya
Acesso em linha:	https://www.frontiersin.org/articles/10.3389/feart.2021.744063/full
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