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Article Navigation >  Acta Sedimentologica Sinica  > 2009  >  27(3): 487-493

SUN Guozhi. The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China[J]. Acta Sedimentologica Sinica, 2009, 27(3): 487-493.
Citation: SUN Guozhi. The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China[J]. Acta Sedimentologica Sinica, 2009, 27(3): 487-493.
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The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China

  • The Key Laboratory of Northwest University Continental Dynamics,Ministry of Education, Department of Geology, Northwest University, Xi′an 710069

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  • Corresponding author: SUN Guozhi
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-06-10
  • The Bogda Mountain located between Junggar basin and TurpanHami basin. Its uplift time has been debated for a long time and is of important geotectonic significance. Based on
    the information of predecessors and the study area, it is considered that the Bogda area was mainly in extensional environment between Early Carboniferous to Middle Permian; in later Pernianearly Triassic period, the particle size, distribution, morphology, composition changes of TurpanHami Basin sediments and stratigraphic contact relationship show that the initial uplifting time of the Bogda mountain took place at late Permian. According to the great changes of time and space about sedimentary facies, ZTR index and sandstone detrital compositions of Xishanyao formation, Sanjianfang formation and Qiketai formation in middle Jurassic epoch on Taibei sag of TurpanHami Basin, it is concluded that the reuplift time of Bogda Mountain took place at late Xishanyao formation, and became the north source supplying area of the TurpanHami Basin. But the maximum uplift amplitude during the Himalayan movement formed the present basinorogen pattern.
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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2009-06-10

The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China

  • The Key Laboratory of Northwest University Continental Dynamics,Ministry of Education, Department of Geology, Northwest University, Xi′an 710069
    Corresponding author: SUN Guozhi
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-06-10

Abstract: The Bogda Mountain located between Junggar basin and TurpanHami basin. Its uplift time has been debated for a long time and is of important geotectonic significance. Based on
the information of predecessors and the study area, it is considered that the Bogda area was mainly in extensional environment between Early Carboniferous to Middle Permian; in later Pernianearly Triassic period, the particle size, distribution, morphology, composition changes of TurpanHami Basin sediments and stratigraphic contact relationship show that the initial uplifting time of the Bogda mountain took place at late Permian. According to the great changes of time and space about sedimentary facies, ZTR index and sandstone detrital compositions of Xishanyao formation, Sanjianfang formation and Qiketai formation in middle Jurassic epoch on Taibei sag of TurpanHami Basin, it is concluded that the reuplift time of Bogda Mountain took place at late Xishanyao formation, and became the north source supplying area of the TurpanHami Basin. But the maximum uplift amplitude during the Himalayan movement formed the present basinorogen pattern.

SUN Guozhi. The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China[J]. Acta Sedimentologica Sinica, 2009, 27(3): 487-493.
Citation: SUN Guozhi. The Preliminary Analysis of the Uplift Time of Bogda Mountain,  Xinjiang, Northwest China[J]. Acta Sedimentologica Sinica, 2009, 27(3): 487-493.
shu

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