A Cretaceous-Eocene depositional age for the Fenghuoshan Group, Hoh Xil Basin: Implications for the tectonic evolution of the northern Tibet Plateau-Reference-Cited by-同舟云学术

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A Cretaceous-Eocene depositional age for the Fenghuoshan Group, Hoh Xil Basin: Implications for the tectonic evolution of the northern Tibet Plateau

Published:2014-03 Issue:3 Volume:33 Page:281-301
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Staisch Lydia M.¹,Niemi Nathan A.¹,Hong Chang²,Clark Marin K.¹,Rowley David B.³,Currie Brian⁴

Affiliation:

1. Department of Earth and Environmental Sciences; University of Michigan; Ann Arbor Michigan USA

2. Institute of Earth Environment; CAS; Xi'an China

3. Department of the Geophysical Sciences; University of Chicago; Chicago Illinois USA

4. Department of Geology and Environmental Earth Science; Miami University; Oxford Ohio USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference118 articles.

1. Strain and rotation rate from GPS in Tibet, Anatolia, and the Altiplano;Allmendinger;Tectonics,2007

2. Characteristics of the Fenghuoshan Group's material and its era discussion;An;Northwestern Geol.,2004

3. La Tectonique de l'Asie;Argand;Proc. Int. Geol. Congr.,1924

4. Stable isotopes of modern water across the Himalaya and eastern Tibetan Plateau: Implications for estimates of paleoelevation and paleoclimate;Bershaw;J. Geophys. Res.,2012

5. Subduction versus accretion of intra-oceanic volcanic arcs: Insight from thermo-mechanical analogue experiments;Boutelier;Earth Planet. Sci. Lett.,2003

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