Morphologic Characteristics of the Miarolitic Alkali Feldspar Granite in
详细信息
- 责任者：Liang Shijing ( Fujian Institute of Geology Survey and Research ; Fuzhou 350003 ; China) ; Wen Feicheng
- 刊名：Geology of Fujian
- 出版年：2010
- 卷期：29(4)
- 关键词：地貌 ; landforms ; 碱长花岗岩 ; alkali feldspar granite ; 地质遗迹 ; geological relics ; 福建 ; Fujian Province
- 页码：p.334-346
- 图表：1 illus., 24 photos, 8 refs.
- 分类号：1400
- issnNo：ISSN1001-3970
- isbnNo：CN35-1080/P
摘要
The Taimushan Mountain is a unique granite peak cluster and stone-egg landform in the low mountains and hills of Southeast China seacoast. The A-type miarolitic alkali feldspar granite of Late Yanshanian is the rock of forming the Taimushan landscape. The NEE and NNW-trending faults,fissures and cleavages are the basic structures of controlling the shape and size of mountain peaks. The weathering denudation, rainfall erosion and gravitational collapse are the major external power of forming the Taimushan landform. At present, the evolution of the landform is in the early stage of late-middle age.