Carbon and oxygen isotopes suggesting deep-water basin deposition associated with hydrothermal events (Shangsi Section, Northwest Sichuan Basin-South China)-Reference-Cited by-同舟云学术

Carbon and oxygen isotopes suggesting deep-water basin deposition associated with hydrothermal events (Shangsi Section, Northwest Sichuan Basin-South China)

Published:2014-02-02 Issue:1 Volume:33 Page:77-85
ISSN:1000-9426
Container-title:Chinese Journal of Geochemistry
language:en
Short-container-title:Chin. J. Geochem.

Author:

Chen Hui,Xie Xi’nong,Mao Kainan,Huang Junhua

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/s11631-014-0661-7.pdf

Reference40 articles.

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2. Chen Hui, Xie Xinong, Hu Chaoyong, Huang Junhua, and Li Hongjing (2012) Geochemical characteristics of Late Permian sediments in the Dalong Formation of the Shangsi Section, Northwest Sichuan Basin in South China [J]. Journal of Geochemical Exploration. 112, 35–53.

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4. Derry L.A., Kaufman A.J., and Jacobsen S.B. (1992) Sedimentary cycling and environmental change in the Late Proterozoic: Evidence from stable and radiogenic isotopes [J]. Geochimica et Cosmochimica Acta. 56, 1317–1329.

5. Feng Shaonan (1991) New knowledge on Dongu Movement [J]. Geoscience. 5, 378–384 (in Chinese).

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