Carbon and oxygen isotopes suggesting deep-water basin deposition associated with hydrothermal events (Shangsi Section, Northwest Sichuan Basin-South China)
Author:
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.
3. Coplen T.B., Kendall C., and Hopple J. (1983) Comparison of stable isotope reference samples [J]. Nature. 302, 236–238.
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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