4.2 Article

Relationship between the later strong gas-charging and the improvement of the reservoir capacity in deep Ordovician carbonate reservoir in Tazhong area, Tarim Basin

期刊

CHINESE SCIENCE BULLETIN
卷 54, 期 17, 页码 3076-3089

出版社

SCIENCE PRESS
DOI: 10.1007/s11434-009-0457-z

关键词

fracture; high-quality carbonate reservoir; deep reservoir; Ordovician; Tazhong No.1 fault zone; Tarim Basin

资金

  1. National Basic Research Program of China [2007CB209500]
  2. National Natural Science Foundation of China [40602016, 40773032]

向作者/读者索取更多资源

Some large-scale oil-gas fields have recently been discovered in marine carbonate in China, especially the significant discoveries in deep reservoir that reveals a favorable exploration prospect. Tazhong area is the first-order tectonic unit in Tarim Basin, where there are nearly trillion cubic meters of natural gas resources in the Ordovician limestone reef flat complex in Lianglitage Formation. The reservoir is shelf edge reef flat complex, characterized by ultra-low porosity, low permeability and strong heterogeneous, with a current burial depth of 4500-6500 m. Studies find that the formation and distribution of deep reservoir of the Lianglitage Formation were controlled not only by the early high-energy sedimentary facies and corrosion, but the fracture network formed by the strong gas-charging process since the Himalayan epoch, which played an important role in optimizing and improving reservoir properties. This paper discusses the relationship between the strong later gas-charging and the improvement of the reservoir capacity in deep Ordovician carbonate reservoir, and also builts the corresponding mechanisms and modes, which is favorable for the prediction and evaluation of the advantageous exploration targets.

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