2012Xinjiang shiyou dizhiRequires access

Relationship Between Present Tectonic Stress Field and Natural Gas Distribution in Kuqa Depression,Tarim Basin

Xiaofeng Sheng

Open publisher page 0 citations

Abstract

The present plane and sectional tectonic stresses were recovered by finite element numerical simulation,their distribution characteristics were summarized,and the relationship between the tectonic stress and the natural gas distribution was analyzed.The results show that in plane,the distribution of maximum principal stress of the sub-salt reservoir in different structural zones is not uniform and characterized by bigger stress in the north than in the south,roughly band-distributing toward near E-W,in the northern part with serious structural compression formed many low-stress areas;in cross section,the maximum principal stress is smaller at the territorial gypsum-salt caprock and its overlying strata,and bigger at the sub-salt strata;and the maximum principal stresses of the Triassic and Jurassic source rocks are generally bigger than that of overlying Cretaceous reservoir.The relative low-stress areas are formed in Kela faulted anticlines and fault blocks in Kelasu structural belt with strong tectonic compression,anticlinal apex and the side of faulted anticline in the upper close to the fault of Keshen zone.The natural gas pools discovered in Kuqa depression up to now are located at the relatively low areas of maximum principal stress.

About this research paper

What this paper is about

The present plane and sectional tectonic stresses were recovered by finite element numerical simulation,their distribution characteristics were summarized,and the relationship between the tectonic stress and the natural gas distribution was analyzed.The results show that in plane,the distribution of maximum principal stress of the sub-salt reservoir in different structural zones is not uniform and characterized by bigger stress in the north than in the south,roughly band-distributing toward near E-W,in the northern part with serious structural compression formed many low-stress areas;in cross section,the maximum principal stress is smaller at the territorial gypsum-salt caprock and its overlying strata,and bigger at the sub-salt strata;and the maximum principal stresses of the Triassic and Jurassic source rocks are generally bigger than that of overlying Cretaceous reservoir.The relative low-stress areas are formed in Kela faulted anticlines and fault blocks in Kelasu structural belt with strong tectonic compression,anticlinal apex and the side of faulted anticline in the upper close to the fault of Keshen zone.The natural gas pools discovered in Kuqa depression up to now are located at the relatively low areas of maximum principal stress.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The present plane and sectional tectonic stresses were recovered by finite element numerical simulation,their distribution characteristics were summarized,and the relationship between the tectonic stress and the natural gas distribution was analyzed.The results show that in plane,the distribution of maximum principal stress of the sub-salt reservoir in different structural zones is not uniform and characterized by bigger stress in the north than in the south,roughly band-distributing toward near E-W,in the northern part with serious structural compression formed many low-stress areas;in cross section,the maximum principal stress is smaller at the territorial gypsum-salt caprock and its overlying strata,and bigger at the sub-salt strata;and the maximum principal stresses of the Triassic and Jurassic source rocks are generally bigger than that of overlying Cretaceous reservoir.The relative low-stress areas are formed in Kela faulted anticlines and fault blocks in Kelasu structural belt with strong tectonic compression,anticlinal apex and the side of faulted anticline in the upper close to the fault of Keshen zone.The natural gas pools discovered in Kuqa depression up to now are located at the relatively low areas of maximum principal stress.

Key concepts: Anticline, Geology, Tectonics, Caprock, Fault (geology), Stress field, Compression (physics), Stress (linguistics)

Related papers

Back to paper searchBrowse research topicsOriginal source
Relationship Between Present Tectonic Stress Field and Natural Gas Distribution in Kuqa Depression,Tarim Basin — Research Paper | ScholarLens