Can a primary remanence be retrieved from partially remagnetized Eocence volcanic rocks in the Nanmulin Basin (southern Tibet) to date the India-Asia collision?-Reference-Cited by-同舟云学术

Can a primary remanence be retrieved from partially remagnetized Eocence volcanic rocks in the Nanmulin Basin (southern Tibet) to date the India-Asia collision?

Published:2015-01 Issue:1 Volume:120 Page:42-66
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Huang Wentao¹²,Dupont-Nivet Guillaume¹²³⁴,Lippert Peter C.⁵⁶,van Hinsbergen Douwe J. J.²,Dekkers Mark J.²,Guo Zhaojie¹,Waldrip Ross⁵,Li Xiaochun⁷,Zhang Xiaoran⁷,Liu Dongdong¹,Kapp Paul⁵

Affiliation:

1. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences; Peking University; Beijing China

2. Department of Earth Sciences; Utrecht University; Utrecht Netherlands

3. Géosciences Rennes; Université de Rennes 1, Campus de Beaulieu; Rennes CEDEX France

4. Institute of Earth and Environmental Science; University of Potsdam; Potsdam-Golm Germany

5. Department of Geosciences; University of Arizona; Tucson Arizona USA

6. Department of Geology and Geophysics; University of Utah; Salt Lake City Utah USA

7. Department of Earth Sciences; University of Hong Kong; Hong Kong China

Funder

U.S. NSF Continental Dynamics

Netherlands Organization for Scientific Research (NWO)

ERC Starting

Marie Curie CIG HIRESDAT

Alexander von Humboldt foundation

Cai Yuanpei Program of the French Ministries of Foreign Affairs and of Higher Education and Research

Chinese Ministry of Education

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JB011599/fullpdf

Reference127 articles.

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