Adv Search
Volume 6 Issue 2
. 
Turn off MathJax
Article Contents
Article Navigation >  Chinese Geographical Science  > 1996  >  6(2): 166-176

Zhong Wei, Wang Jianmin. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE[J]. Chinese Geographical Science, 1996, 6(2): 166-176.
Citation: Zhong Wei, Wang Jianmin. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE[J]. Chinese Geographical Science, 1996, 6(2): 166-176.
shu

PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE

  • 1.

    Department of Geography, Xinjiang University, Urumqi 830046, PRC;

  • 2.

    Department of Geography Science, Lanzhou University, Lanzhou 730000, PRC

  • Received Date: 1995-05-01
  • Publish Date: 1996-06-20
  • A great number of geologic records has shown that the climatic environment in Xinjiang in the Holocene was mainly characterized by warm-dry, although alternated with sub-fluctuations, several important boundaries of environmental changes can also be determined as follows:12, 000 a B.P., 9000 a B.P., 3000 a B.P., 1500 a B.P.and 400 a B.P.Since the Holocene, Xinjiang has undergone the influence of two kinds of environmental development patterns(the westerly type and the monsoon type), so the hydro-thermal disposal here was much more complicated.Generally speaking, the neoglacials of Xinjiang are characteristics of cold(cool)-humid and in the Climatic Optimal, it is dominated by warm-humid conditions in spite of being intercalated several sub-fluctuations of warm-dry intervals.
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Get Citation
PDF
XML

Article Metrics

Article views(1037) PDF downloads(743) Cited by()

Proportional views
Related

PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE

  • 1. Department of Geography, Xinjiang University, Urumqi 830046, PRC;
  • 2. Department of Geography Science, Lanzhou University, Lanzhou 730000, PRC
  • Received Date: 1995-05-01
  • Publish Date: 1996-06-20

Abstract: A great number of geologic records has shown that the climatic environment in Xinjiang in the Holocene was mainly characterized by warm-dry, although alternated with sub-fluctuations, several important boundaries of environmental changes can also be determined as follows:12, 000 a B.P., 9000 a B.P., 3000 a B.P., 1500 a B.P.and 400 a B.P.Since the Holocene, Xinjiang has undergone the influence of two kinds of environmental development patterns(the westerly type and the monsoon type), so the hydro-thermal disposal here was much more complicated.Generally speaking, the neoglacials of Xinjiang are characteristics of cold(cool)-humid and in the Climatic Optimal, it is dominated by warm-humid conditions in spite of being intercalated several sub-fluctuations of warm-dry intervals.

Zhong Wei, Wang Jianmin. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE[J]. Chinese Geographical Science, 1996, 6(2): 166-176.
Citation: Zhong Wei, Wang Jianmin. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE[J]. Chinese Geographical Science, 1996, 6(2): 166-176.
shu

    HTML

Catalog

    Copyright © Editorial office of Chinese Geographical Science

    Tel: +86-0431-85542219   Email: egeoscien@neigae.ac.cn  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return