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塔中隆起NNE向走滑断裂特征及形成机制

杨勇 汤良杰 郭颖 谢大庆

中国地质2016,Vol.43Issue(5):1569-1578,10.
中国地质2016,Vol.43Issue(5):1569-1578,10.DOI:10.12029/gc20160507

塔中隆起NNE向走滑断裂特征及形成机制

Deformation characteristics and formation mechanism of NNE-trending strike-slip faults in Tazhong Uplift

杨勇 1汤良杰 2郭颖 3谢大庆4

作者信息

  • 1. 中国地质科学院地质力学研究所,北京100081
  • 2. 中国石油大学油气资源与探测国家重点实验室,北京102249
  • 3. 中国石油大学盆地与油藏研究中心,北京102249
  • 4. 中国石油大学油气资源与探测国家重点实验室,北京102249
  • 折叠

摘要

Abstract

In this study, the correlation method of structural factors and structural analysis were used to determine the formation mechanism of NNE-trending strike-slip faults in the Tazhong Uplift. The interpretation of 2D and 3D seismic data revealed deformation characteristics of the NNE-striking faults and determined their formation mechanism. NNE-trending strike-slip faults exhibit vertical superposition of compresso-shear faults and tenso-shear faults in seismic profiles. They have experienced two stages of activities:the late Ordovician compresso-shear faulting and the late Silurian-middle Devonian tenso-shear faulting. The formation of the NNE-trending strike-slip faults was controlled by the pre-existing basement weak zone and the evolution of the orogenic belts around Tarim plate. At the end of Middle Ordovician, a NS-trending compressive stress was generated by the subduction and closure of the ocean basin on the south margin of Tarim plate, and it acted on the NE-trending basement weak zone, resulting in the formation of NNE-trending strike-slip faults. Meanwhile, the compressive stress from the northwest margin of Tarim plate vertically acted on the NNE-striking strike-slip fault, leading to the compresso-shear deformation. In late Silurian-middle Devonian period, the NS-trending compressive stress continually acted on the strike-slip faults, resulting in continued strike-slip deformation. Moreover, the extensional stress from the northwest margin of Tarim plate vertically acted on the NNE-striking strike-slip fault, leading to the tenso-shar deformation.

关键词

塔中隆起/断裂体系/走滑断裂/雁列式断层/形成机制

Key words

Tazhong uplift/fault system/strike-slip fault/en-echelon faults/formation mechanism

分类

天文与地球科学

引用本文复制引用

杨勇,汤良杰,郭颖,谢大庆..塔中隆起NNE向走滑断裂特征及形成机制[J].中国地质,2016,43(5):1569-1578,10.

基金项目

国家自然科学基金项目(4097209、41572105)和国家专项“深部探测与实验研究”(SinoProbe-08-01)联合资助。 (4097209、41572105)

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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