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Volume 42 Issue 5
Sep.  2020
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2020  >  42(5): 756-766
CHEN Hanlin, HUANG Weikang, LI Yong, ZHANG Fengqi, WU Hongxiang, YANG Zhilin, HUANG Shaoying, YANG Shufeng. Provenance analysis of Sinian sediments on the northwestern margin of Tarim Basin and its restriction on basin types[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(5): 756-766. doi: 10.11781/sysydz202005756
Citation: CHEN Hanlin, HUANG Weikang, LI Yong, ZHANG Fengqi, WU Hongxiang, YANG Zhilin, HUANG Shaoying, YANG Shufeng. Provenance analysis of Sinian sediments on the northwestern margin of Tarim Basin and its restriction on basin types[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(5): 756-766. doi: 10.11781/sysydz202005756
shu

Provenance analysis of Sinian sediments on the northwestern margin of Tarim Basin and its restriction on basin types

doi: 10.11781/sysydz202005756
  • 1.

    School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China

  • 2.

    Research Center for Structures in Oil and Gas-bearing Basins, Ministry of Education, Hangzhou, Zhejiang 310027, China

  • 3.

    Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Kuerle, Xinjiang 841000, China

  • Received Date: 2020-05-21
  • Rev Recd Date: 2020-07-28
  • Publish Date: 2020-09-28
    Abstract
  • The Neoproterozoic is a very important stage in the global tectonic evolution, which experienced the amalgamation and break-up of the Rodinia. The Nanhua and Sinian strata in the Tarim Basin, which is one of the three major craton basins, have recorded a great deal of information about the tectonic attributes and plate dynamics of the basin in the Neoproterozoic. These are also the key strata for deep oil and gas exploration in the Tarim Craton Basin. Based on field investigations and studies of sedimentary characteristics, this paper studies the U-Pb dating of detrital zircons and provenance of sediments from the Sinian strata outcropped on the northwestern margin of the Tarim Basin. The age distribution of detrital zircons from the Sugetebrak Formation have five peaks in age of about 2 600, 2 300, 2 000-1 800, 790-730 and 620 Ma. The detrital zircons with peak ages of 2 600, 2 300 and 2 000-1 800 Ma are from the Neoarchean-Mesoproterozoic basement within the Tarim Craton, the detrital zircons with peak ages of 790-730 Ma may be derived from magmatic rocks formed by rifting during the late Neoproterozoic in the Tarim Basin, and the zircons with a peak age of 620 Ma were directly derived from magmatism at the time of formation deposition. These results suggest that the clastic material may have originated in the Tarim Basin itself. In view of the fault depression to depression structure on seismic profile, the rapidly filled turbidite sedimentary construction in the Nanhua strata, the transformation of Sinian strata from a clastic rock sequence to a marine carbonate sequence, and the magmatism during the sedimentary period of the Sinian Sugetebrak Formation, it is concluded that the northwestern margin of the Tarim Basin experienced the transition from fault-depression to rift subsidence during the Sinian.

     

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