中国花岗岩地貌的类型特征与演化
收稿日期: 2006-11-21
修回日期: 2007-05-08
网络出版日期: 2007-07-25
The Type and Evolution of the Gr anite Landforms in China
Received date: 2006-11-21
Revised date: 2007-05-08
Online published: 2007-07-25
崔之久, 杨建强, 陈艺鑫 . 中国花岗岩地貌的类型特征与演化[J]. 地理学报, 2007 , 62(7) : 675 -690 . DOI: 10.11821/xb200707001
With the subtropical monsoon climate in southern China, the planation surface and the crust of weathering developed into many particular granite landform types, such as that on Mt. Huangshan and Mt. Sanqingshan, as a result of the uplift and down-cut in the following tectonic movements. In this paper, the temporal and spatial development discipline of the granite crust of weathering and landform was discussed, and the close relationship between the landform age and planation surface was studied. The connections of the granite landform and the crust of weathering were also put forward in different uplift background. Based on that, the uplift extent of massifs can be presumed, which would be ~200 m at coastal region, and increase to 1600-2000 m at the Nanling Mountains or Dabie Mountain and Funiu Massif.
Key words： China; granite; landform; planation surface; climate; tectonic movements
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