Fluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin, China-Reference-Cited by-同舟云学术

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Fluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin, China

Published:2014-12-17 Issue:3 Volume:15 Page:483-498
ISSN:1468-8115
Container-title:Geofluids
language:en
Short-container-title:Geofluids

Author:

Jiang L.¹²,Pan W.³,Cai C.¹,Jia L.¹,Pan L.⁴,Wang T.¹,Li H.¹,Chen S.¹⁵,Chen Y.¹

Affiliation:

1. Key Lab of Petroleum Resources; Institute of Geology and Geophysics; Chinese Academy of Sciences; Beijing China

2. Department of Geology and Geophysics; School of Environmental Sciences; University of Liverpool; Liverpool UK

3. Tarim Oilfield Company; PetroChina; Korla Xinjiang China

4. PetroChina Hangzhou Research Institute of Geology; Hangzhou China

5. Energy Resource Department; China University of Geosciences; Beijing China

Funder

Special Major Project on Petroleum Study

China National Funds

Natural Science Foundation of China

China Postdoctoral Science Foundation

Publisher

Wiley

Subject

General Earth and Planetary Sciences

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/gfl.12125/fullpdf

Reference54 articles.

1. Isotope signatures associated with early meteoric diagenesis;Allan;Sedimentology,1982

2. Origin and migration of brines from Paleozoic strata in Central Tarim, China: constraints from 87Sr/86Sr, δD, δ18O and water chemistry;Cai;Applied Geochemistry,2001a

3. Thermochemical sulphate reduction in Cambro-Ordovician carbonates in Central Tarim;Cai;Marine and Petroleum Geology,2001b

4. Thermochemical sulphate reduction and the generation of hydrogen sulphide and thiols (mercaptans) in Triassic carbonate reservoirs from the Sichuan Basin, China;Cai;Chemical Geology,2003

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