塔里木盆地西北缘四石厂地区下二叠统沉积与物源记录及其反映的构造演化

郭春涛; 高剑; 李忠

doi:10.3799/dqkx.2017.595

Volume 43 Issue 11

Nov. 2018

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Article Navigation > Earth Science > 2018 > 43(11): 4149-4168

Guo Chuntao, Gao Jian, Li Zhong, 2018. Depositional and Provenance Records of Lower Permian Sandstones from Sishichang Area, Northwestern Tarim Basin: Implications for Tectonic Evolution. Earth Science, 43(11): 4149-4168. doi: 10.3799/dqkx.2017.595

Citation:

Guo Chuntao, Gao Jian, Li Zhong, 2018. Depositional and Provenance Records of Lower Permian Sandstones from Sishichang Area, Northwestern Tarim Basin: Implications for Tectonic Evolution. Earth Science, 43(11): 4149-4168. doi: 10.3799/dqkx.2017.595

Citation:

Guo Chuntao, Gao Jian, Li Zhong, 2018. Depositional and Provenance Records of Lower Permian Sandstones from Sishichang Area, Northwestern Tarim Basin: Implications for Tectonic Evolution. Earth Science, 43(11): 4149-4168. doi: 10.3799/dqkx.2017.595

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Depositional and Provenance Records of Lower Permian Sandstones from Sishichang Area, Northwestern Tarim Basin: Implications for Tectonic Evolution

doi: 10.3799/dqkx.2017.595

Guo Chuntao^{1,2,3
,},
Gao Jian^2,4,
Li Zhong^{2
,
,}

1.
College of Architecture and Surveying Engineering, Shanxi Datong University, Datong 037003, China
2.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
3.
Daqing Oilfield of Personnel Development Institute, China National Petroleum Corporation, Daqing 163453, China
4.
Beijing Geothermal Research Institute, Beijing 100143, China

Received Date: 2017-12-17
Publish Date: 2018-11-15

Abstract

Abstract

Carboniferous-Permian is the critical tectonic evolution period of the South Tianshan Ocean and the northern margin of Tarim basin. The Carboniferous-Permian outcrop, located in the northwestern margin of Tarim basin, near the South Tianshan orogen, is well exposed in the Sishichang area, and is selected to analyze this problem. Based on depositional system, sandstone skeleton component, heavy minerals, especially detrial zircon geochronology analysis by LA-ICP-MS in situ U-Pb and Lu-Hf isotope, this study further explores provenance, tectonic evolution and its geodynamic mechanism about the Tarim basin and the periphery orogenic belt. The results show that sandstone grains are dotted in the continental block provenances and the merger of fields for mature rocks with stable frameworks; the main proportions of heavy mineral assemblages are the stable heavy minerals. These results reflect that tectonic setting may be stable. The geochronological samples show multiphase tectono-thermal events with age groups of 407-501 Ma, 755-873 Ma, 889-1 129 Ma, 1 792-2 079 Ma, and 2 393-2 496 Ma. Compared with the potential source areas, the main provenance may be the Tarim palaeohigh. The redeposition of pre-Permian strata in the Tarim basin, associated with the erosion source in the Kunlun-Altun orogen, may also have some contribution. In other words, although the South Tianshan Ocean may have been closed, the South Tianshan orogenic belt did not uplift on a large scale until the Asselian. And the tectonic pattern and provenance of northwestern margin of Tarim basin changed little because of the closure. Referring to the previous data, it is concluded that the single source of the Tarim palaeohigh has developed into the dual sources of the Tarim basin and orogenic belt form Asselian to Sakmarian, and the provenance system of Keping area changes greatly. Furthermore, the South Tianshan Ocean, closed in Carboniferous, began to uplift in Sakmarian, and became an important source to the northwestern margin of Tarim basin.
- northwestern margin of Tarim basin,
- provenance system,
- tectonic evolution,
- sedimentology

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