Carbon isotopes, sulfur isotopes, and trace elements of the dolomites from the Dengying Formation in Zhenba area, southern Shaanxi: Implications for shallow water redox conditions during the terminal Ediacaran-Reference-Cited by-同舟云学术

Carbon isotopes, sulfur isotopes, and trace elements of the dolomites from the Dengying Formation in Zhenba area, southern Shaanxi: Implications for shallow water redox conditions during the terminal Ediacaran

Published:2015-04-30 Issue:7 Volume:58 Page:1107-1122
ISSN:1674-7313
Container-title:Science China Earth Sciences
language:en
Short-container-title:Sci. China Earth Sci.

Author:

Chen YaLi,Chu XueLei,Zhang XingLiang,Zhai MingGuo

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s11430-015-5071-0.pdf

Reference80 articles.

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3. Banner J L, Hanson G N, Meyers W J. 1988. Rare earth element and Nd isotopic variations in regionally extensive dolomites from the Burlington-Keokuk Formation (Mississippian): Implications for REE mobility during carbonate diagenesis. J Sediment Res, 58: 415–432

4. Berkner L V, Marshall L. 1965. On the origin and rise of oxygen concentration in the Earth’s atmosphere. J Atmos Sci, 22: 225–261

5. Bowring S A, Grotzinger J P, Condon D J, et al. 2007. Geochronologic constraints on the chronostratigraphic framework of the Neoproterozoic Huqf Supergroup, Sultanate of Oman. Am J Sci, 307: 1097–1145

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