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    Volume 45 Issue 1
    Jan.  2020
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    Article Contents
    Li Tian, Xie Guoai, Zhang Jin, Qu Junfeng, Zhang Beihang, Zhao Heng, Tian Rongsong, Aimierding·Aierken, Li Fahao, 2020. Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution. Earth Science, 45(1): 211-225. doi: 10.3799/dqkx.2018.342
    Citation: Li Tian, Xie Guoai, Zhang Jin, Qu Junfeng, Zhang Beihang, Zhao Heng, Tian Rongsong, Aimierding·Aierken, Li Fahao, 2020. Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution. Earth Science, 45(1): 211-225. doi: 10.3799/dqkx.2018.342

    Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution

    doi: 10.3799/dqkx.2018.342
    • Received Date: 2018-09-26
    • Publish Date: 2020-01-15
    • The fault structure is very complex, with several extension directions including the north-south, east-west, north-east and north-west in Langshan area, Inner Mongolia. In this study, we conducted the geometrical morphology, fault movement property and structural stress field analyses on the N-S trending fault, combining with field investigation and stereographic projection, to reveal the regional structural stress field and tectonic evolution history in Langshan area. Our preliminary results show that the N-S trending fault in the study area has experienced at least two phases of significant tectonic events. The first phase is in the Late Permian, because a collision collage movement due to the northward movement of North China Craton and the southward movement of Siberia plate produced nearly horizontal compressive tectonic stress field with principal stress axis sigma 1 for north by east 10° or so, plunging to the north, and with dip angle of 15°-20°. As aresult the Langshan mountain region developed a rupture system, which consisted of nearly east-west direction compressive tectonic belt and reverse fault, near the north-east direction of the predominantly left strike-slip faults, near north-west direction of the predominantly right lateral strike-slip faults and nearly north-south extensional fault.These first formed fault systems also have controlled and constrained subsequent tectonic activity in the region.The second phase of tectonic stress field was generated by the subduction of the palaeo-pacific plate from the Jurassic to the Asian continent.The tectonic stress field of the principal stress axis sigma 1 is northeast-southwest, plunging to about 150° and with dip angle of 10°-20°.The effect of the second phase of the tectonic stress field made the early fault tectonics move again, so that the early north-south fault was turned from the original tensile fracture plane to the left-lateral strike-slip, early east-west fracture from compressional structural surface to left-lateral strike-slip, early north-east left-lateral strike-slip surface shifted to the compressive surface and the fold extended direction. The early north-west was converted to a rupture property.

       

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