地理学报

Acta Geographica Sinica ›› 1992, Vol. 47 ›› Issue (5): 430-440.doi: 10.11821/xb199205006

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THE NEOTECTONIC ANALYSIS OF THE QUATERNARY DIPOSITS AND STEPPED LANDFORMS IN MT. YULONGXUESHAN-MT. CANGSHAN REGION

Chen Fubin1, Chen Jiliang1, Xu Xifeng2, Ge Tongmin3, Liana Chunvan3, Fan Limin3   

  1. 1. Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu　600015;
    2. Hydrogcological & Engineer Geological Team, Sichuan Burcau of Geology & Minerals, Chengdu　610072;
    3. Heodyuaters of South Sea Investigation, Chinese Ministry of Ministry of Geology & Minerals, Guangzhou 510760
  • Online:1992-09-15 Published:1992-09-15

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Abstract: Mt Yulongxue (5596 meters a.b.l.) and Mt. Cangshan (4122 meters a.b.l.) which are located in the southeast of Tibet Plateau and the central part of the Hengduan Mountain System are major peaks in the northwest part of Yunnan province.

Key words: Neotectonic landform, Pal oplanation surface, Neotectonic period, Jian-chuan laterite, Songmaopo formation