Evidence for a gradual rise of oxygen between 2.6 and 2.5 Ga from Mo isotopes and Re-PGE signatures in shales

Wille, Martin; Kramers, Jan; Nägler, Thomas; Beukes, N; Schröder, S; Meisel, Th; Lacassie, J; Voegelin, Andrea (2007). Evidence for a gradual rise of oxygen between 2.6 and 2.5 Ga from Mo isotopes and Re-PGE signatures in shales. Geochimica et cosmochimica acta, 71(10), pp. 2417-2434. New York, N.Y.: Elsevier Science 10.1016/j.gca.2007.02.019

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Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences
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UniBE Contributor:

Wille, Martin; Kramers, Jan Dirk; Nägler, Thomas and Vögelin, Andrea

ISSN:

0016-7037

Publisher:

Elsevier Science

Language:

English

Submitter:

Thomas Nägler

Date Deposited:

04 Oct 2013 15:00

Last Modified:

09 May 2014 20:34

Publisher DOI:

10.1016/j.gca.2007.02.019

Web of Science ID:

000246699600001

URI:

https://boris.unibe.ch/id/eprint/25911 (FactScience: 62271)

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