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    ZHOU Jia-yun, LI Yong, LI Ya-lin. Analysis on Triassic sedimentary environment in Tanggulashan area, Tibet[J]. Northwestern Geology, 2004, 37(2): 25-29.
    Citation: ZHOU Jia-yun, LI Yong, LI Ya-lin. Analysis on Triassic sedimentary environment in Tanggulashan area, Tibet[J]. Northwestern Geology, 2004, 37(2): 25-29.

    Analysis on Triassic sedimentary environment in Tanggulashan area, Tibet

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    • Received Date: December 15, 2003
    • Revised Date: January 16, 2004
    • Published Date: June 04, 2004
    • In Tria ssic period,Qiangbei-Changdu area is a paraplat forma reaplaced between Jinsha jiang river oceanic basic and Bangong lake-Nujiang river oceanic basic. Tanggula shan area is an excessive a rea between Qiangtang area and Changdu area,which is situated on east of Qiangtang area,and is located next to the west of Chuangdu aera. Tanggula shan area may provides both Qiangtang area and Chuangdua rea with important reference material through reseaching its sedimentary environment.
    • 青海省区调综合大队. 1:20万区域地质调查报告(雁石坪幅、索加幅)[R].1993.
      饶荣标,等. 青藏高原的三叠系[M].北京:地质出版社, 1987.
      刘世坤,徐开峰,等. 西藏羌北-昌都地区三叠纪的海侵事件及印支运动的期次[J]. 西藏地质, 1995,(2).
      青海省地质矿产局. 青海省岩石地层[M]. 武汉:中国地质大学出版社,1997.
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