Application of Stable Strontium Isotope Geochemistry and Fluid Inclusion Microthermometry to Studies of Dolomitization of the Deeply Buried Cambrian Carbonate Successions in West-Central Tarim Basin, NW China-Reference-Cited by-同舟云学术

Application of Stable Strontium Isotope Geochemistry and Fluid Inclusion Microthermometry to Studies of Dolomitization of the Deeply Buried Cambrian Carbonate Successions in West-Central Tarim Basin, NW China

Published:2019-01-28 Issue:1 Volume:30 Page:176-193
ISSN:1674-487X
Container-title:Journal of Earth Science
language:en
Short-container-title:J. Earth Sci.

Author:

Ngia Ngong Roger^ORCID,Hu Mingyi^ORCID,Gao Da,Hu Zhonggui,Sun Chun-Yan

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/article/10.1007/s12583-017-0954-y/fulltext.html

Reference61 articles.

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4. Cai, C. F., Li, K. K., Li, H. T., et al., 2008. Evidence for Cross Formational Hot Brine Flow from Integrated 87Sr/86Sr, REE and Fluid Inclusions of the Ordovician Veins in Central Tarim, China. Applied Geochemistry, 23(8): 2226–2235. https://doi.org/10.1016/j.apgeochem.2008.03.009

5. Cai, C. F., Xie, Z. Y., Worden, R. H., et al., 2004. Methane-Dominated Thermochemical Sulphate Reduction in the Triassic Feixianguan Formation East Sichuan Basin, China: Towards Prediction of Fatal H2S Concentrations. Marine and Petroleum Geology, 21(10): 1265–1279. https://doi.org/10.1016/j.marpetgeo.2004.09.003

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