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Natural Gas Geoscience ›› 2011, Vol. 22 ›› Issue (4): 618-627.doi: 10.11764/j.issn.1672-1926.2011.04.618

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The Heavy Minerals and Provenances of the Upper Triassic Xujiahe Formation in Sichuan Basin

SHI Zhen-Sheng, WANG Xiu-Qin, WU Chang-Jiang   

  1. 1.China University of Mining and Technology,Beijing 100083,China；
    2.Langfang Branch of PetroChina Research Institute of Petroleum Exploration and Development,Langfang 065007,China；
    3.PetroChina Southwest Oil and Gas Field Company,Chengdu 610051,China
  • Received:2011-05-05 Revised:2011-06-03 Online:2011-08-10 Published:2011-08-10

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Abstract:

Hyperstable heavy minerals with little diversity in different members were dominated in the upper Triassic Xujiahe Formation of Sichuan basin.Heavy mineral measurement is not only helpful to accurate restoration of depositional systems and ancient water systems,but also reveal the rock\|tectonic attribute of Longmen Shan and recovery of tectonic uplift history.Q\|cluster and principal factor show that the parent rock in the Xujiahe Formation is dominated by sedimentary rocks and low\|level metamorphic rocks,as well as low content of high-grade metamorphic rocks.The content of high-grade metamorphic rocks increases from section bottom to top.ZTR index shows that 4 main source areas in the late Triassic Sichuan basin are located in south-west,north\|west,north-east and south\|east of Sichuan basin,respectively.The distribution of source areas exist inherited.Based on tectonic belt and sedimentology of previous research,the Longmen Shan fold belt begin to form at late Triassic Period.At the second phase of Xujiahe Formation,the northern section of Longmen Shan had been exposed and eroded,but the southern section was still underwater or not yet uplifted.At the fourth phase,the northern section of Longmen Shan continued uplift and suffered erosion,whereas the southern section started uplift and erosion and provided the sediments toward the basin.At the sixth phase,the Longmen Shan was uplifted fully and provided sediments to the basin.

Key words: Sichuan basin, Upper Triassic, Heavy mineral, Provenance, Tectonic evolution.

CLC Number: 

  • TE122.1+1


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