Increasing Nd isotopic ratio of Asian dust indicates progressive uplift of the north Tibetan Plateauince the middle Miocene

Li, G.; Pettke, Thomas; Chen, J. (2011). Increasing Nd isotopic ratio of Asian dust indicates progressive uplift of the north Tibetan Plateauince the middle Miocene. Geology, 39(3), pp. 199-202. Boulder, Colo.: Geological Society of America 10.1130/G31734.1

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Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences
08 Faculty of Science > Institute of Geological Sciences > Rock-Water Interaction

UniBE Contributor:

Pettke, Thomas

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

0091-7613

Publisher:

Geological Society of America

Language:

English

Submitter:

Factscience Import

Date Deposited:

04 Oct 2013 14:28

Last Modified:

12 May 2020 08:54

Publisher DOI:

10.1130/G31734.1

Web of Science ID:

000287374900004

URI:

https://boris.unibe.ch/id/eprint/10548 (FactScience: 216447)

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