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The origin of fluid in calcite veins and its implications for hydrocarbon accumulation in the Shunnan-Gucheng area of the Tarim Basin, China

  • Published:2020-12 Issue:6 Volume:5 Page:341-353
  • ISSN:2468-256X
  • Container-title:Journal of Natural Gas Geoscience
  • language:en
  • Short-container-title:Journal of Natural Gas Geoscience

Author:

Li Huili,You Donghua,Han Jun,Qian Yixiong,Sha Xuguang,Xi Binbin

Funder

Technology Department Program of SINOPEC

Chinese Academy of Sciences Strategic Leading Science and Technology Project

Publisher

Elsevier BV

Reference61 articles.

1. The fracture characteristics of Ordovician limestone in Tazhong No.1 fault belt;Wu;Acta Pet. Sin.,1999

2. Structural diagenesis in carbonate fault damage zone: a case study of the No.1 fault zone in the Tarim Basin;Zhang;Acta Petrol. Sin.,2016

3. Geochemical study of calcite veins in the Silurian and Devonian of the Barrandian Basin (Czech Republic): evidence for widespread post-Variscan fluid flow in the central part of the Bohemian Massif;Suchy;Sediment. Geol.,2000

4. C and O isotope systematics in hydrothermal calcite-fluorite veins: implications for fluid-rock reaction and geochronology;Barker;Chem. Geol.,2009

5. Timing and mechanism of late-Pleistocene calcite vein formation across the Dead Sea Fault Zone, northern Israel;Nuriel;J. Struct. Geol.,2012
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