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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.
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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.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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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.
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