Volume 25 Issue 6
Dec.  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(6): 1025-1035
LYU Baofeng, WU Qiong, YANG Yongqiang, 2019. CHARACTERISTICS OF THE 'BRUSH STRUCTURE SYSTEM' AND A PRIMARY ANALYSIS ON ITS FORMATION DYNAMIC MECHANISM IN THE EASTERN CENTRAL UPLIFT BELT, TARIM BASIN. Journal of Geomechanics, 25 (6): 1025-1035. DOI: 10.12090/j.issn.1006-6616.2019.25.06.085
Citation: LYU Baofeng, WU Qiong, YANG Yongqiang, 2019. CHARACTERISTICS OF THE "BRUSH STRUCTURE SYSTEM" AND A PRIMARY ANALYSIS ON ITS FORMATION DYNAMIC MECHANISM IN THE EASTERN CENTRAL UPLIFT BELT, TARIM BASIN. Journal of Geomechanics, 25 (6): 1025-1035. DOI: 10.12090/j.issn.1006-6616.2019.25.06.085
shu

CHARACTERISTICS OF THE "BRUSH STRUCTURE SYSTEM" AND A PRIMARY ANALYSIS ON ITS FORMATION DYNAMIC MECHANISM IN THE EASTERN CENTRAL UPLIFT BELT, TARIM BASIN

doi: 10.12090/j.issn.1006-6616.2019.25.06.085
  • 1.

    School of Marine Sciences, Sun Yat-sen University, Zhuhai 519082, Guangdong, China

  • 2.

    State Key Laboratory of Geological Processes and Mineral Resource, China University of Geoscience, Beijing 100083, China

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  • Received: 2019-06-22
  • Revised: 2019-10-31
  • Published: 2019-12-31
    Abstract
  • Fault is the main type of structural deformation in the eastern part of the middle uplift zone in the Tarim basin, and it is also an important factor controlling hydrocarbon accumulation and distribution. Based on the structural system theory of Professor J.S.Lee, and through the comprehensive analysis of geometry, kinematics and dynamics characteristics of faults in the eastern part of central uplift belt in the Tarim basin, the geodynamics models of "brush structural system" are discussed in this paper. Research results show that:since the early paleozoicera, affected by the three orogenic belts of the Southern Tianshan mountain in the north, the Kunlun mountain in the southwest and the Altun mountain in the southeast and along with the evolutionary process of the three great extension-convergent tectonic cycles, faults, such as the Central Tarim Fault Ⅰ, the Central Tarim Fault 10, the Central Tarim Fault Ⅱ, the Katak southern edge faults and so on, were generated successively and had been active many times. They present as "Y" type structure on the profile, and constrict to the SE direction and spread out to the NW direction on plane, forming as the "brush structure system" together with the Tangnan strike-slip fault and Cheerchen strike-slip fault on the south side. Ever since the early time of Caledonian orogeny, the "brush structure system" experienced two regional stress field conversion history of the tenso-shear stage (early Caledonian orogeny)→ the compresso-shear stage(moddle Caledonian orogeny)→the tenso-shear stage(early Hercynian orogeny) and the compresso-shear stage(late Hercynian orogeny), and basically finalized the design by the time of late Hercynian orogeny, in the meantime, many lower generation faults of NE trend and NEE trend were generated.

     

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