| 青藏高原隆起与中国自然环境的演化 |
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| 引用本文： | 赵清. 青藏高原隆起与中国自然环境的演化[J]. 徐州师范大学学报(自然科学版), 1991, 0(3) |
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| 作者姓名： | 赵清 |
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| 作者单位： | 徐州师范学院地理系 |
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| 摘 要： | 青藏高原隆起最终奠定了我国现代地貌格局与地形特点,我国现代季风环流的建立与高原隆起有直接关系。我国现代季风与第三纪末的古季风在成因与强度上有质的差异。伴随高原的隆起,我国自然地理环境从上新世末的以行星风系为主的区域分异演变成现今的三大地理区。
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| 关 键 词： | 现代季风 古季风 地域分异 |
THE UPLIFT OF THE QINGHAI-XIZANG PLATEAU AND EVOLUTION OF PHYSICOGEOGRAPHICAL ENVIRONMENTS OF CHINA |
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| Zhao Qing. THE UPLIFT OF THE QINGHAI-XIZANG PLATEAU AND EVOLUTION OF PHYSICOGEOGRAPHICAL ENVIRONMENTS OF CHINA[J]. Journal of Xuzhou Normal University(Natural Science Edition), 1991, 0(3) |
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| Authors: | Zhao Qing |
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| Abstract: | The nodern geonorphological pattern and the characters of kabdfirms in China are cintrilled by the uplift of the Qinghai - Xizang plateau. And the formation of the modern monsoon circulation in the East Asia ate directly related with the uplift of the plateau. The modern monxoon and the late Tretiaryan-cient monsoon are different from each other on formation and intensity, with the uplift of the plateau , the present three great physicogeographical regions aregradually evolved from the late pliocene physicogeographical environment. which wascontrolled by the planetrary wind system. |
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| Keywords: | mondern monsoon ancient monsoon reginal division |
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