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2016 Vol. 49, No. 4
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HAO Qiang, LIN Liangbiao, YU Yu, GAO Jian, QIAN Lijun. Research on Provenance and Characteristics of Sandstone Composition of Xujiahe Formation in Southern Sichuan[J]. Northwestern Geology, 2016, 49(4): 110-120.
Citation: HAO Qiang, LIN Liangbiao, YU Yu, GAO Jian, QIAN Lijun. Research on Provenance and Characteristics of Sandstone Composition of Xujiahe Formation in Southern Sichuan[J]. Northwestern Geology, 2016, 49(4): 110-120.
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Research on Provenance and Characteristics of Sandstone Composition of Xujiahe Formation in Southern Sichuan

  • 1.

    Department of Resource Prospection and Civil Gngineering, Engineering & Technical College of Chengdu University of Technology, Leshan 614000, Sichuan, China;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 2.

    State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 3.

    Department of Resource Prospection and Civil Gngineering, Engineering & Technical College of Chengdu University of Technology, Leshan 614000, Sichuan, China

Received Date:  05 February 2016
Revised Date:  08 June 2016
Publish Date:  15 December 2016
    Abstract
  • Upper Triassic Xujiahe Formationis the major oil and gas exploration reservoir in southern Sichuan. Through analyzing the detrital components and heavy mineral, the several provenances have been existed in the Xujiahe Formation of southern Sichuan, inluding LongmenMoutain, Kangdian old land, Xuefeng ancient land and Qianzhong ancient land. LongmenMoutain provenance mainly affects the northwest part of this studying area, providing magmatic debris and metamorphic debris, and developing a NW-SE direction (short-axis) delta sedimentary system. The clastic rocks are occurred in the north and southeast parts of this studying area, including mudstone debris, silt debris and metamorphic debris, which are mainly sourced from Xuefeng ancient land with the development of a SE-NW direction (long-axis) delta sedimentary system. The southwest and south parts of study area are controlled by Kangdian ancient land and Qianzhong ancient land, which are supported by the evidences of the heavy minerals study.
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