Types and spatial combinations of Danxia landform of Fangyan in Zhejiang Province
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- 作者：Jie Ouyang (1)
Cheng Zhu (1)
Hua Peng (2)
Jinbiao Yu (1)
Lan Li (1)
Riliang Zhou (3)
Guangsheng Zhang (1)
Guangyao Zhu (4)
Zhongxuan Li (1)
Yishun Zhong (5)
Qing Zhu (1)
Wen Lv (1)
Yongqi Hu (6)
Chaogui Zheng (5)
Zhenrong Lv (6)
Chang Hu (6)
Honglin Wu (7)
Longsheng Xu (1) - 关键词：Fangyan of Zhejiang Province ; Danxia landform ; Fangyan Formation (K1 f)
- 刊名：Journal of Geographical Sciences
- 出版年：2009
- 出版时间：October 2009
- 年：2009
- 卷：19
- 期：5
- 页码：631-640
- 全文大小：881KB
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Cheng Zhu (1)
Hua Peng (2)
Jinbiao Yu (1)
Lan Li (1)
Riliang Zhou (3)
Guangsheng Zhang (1)
Guangyao Zhu (4)
Zhongxuan Li (1)
Yishun Zhong (5)
Qing Zhu (1)
Wen Lv (1)
Yongqi Hu (6)
Chaogui Zheng (5)
Zhenrong Lv (6)
Chang Hu (6)
Honglin Wu (7)
Longsheng Xu (1)
1. School of Geographic and Oceanographic Sciences of Nanjing University, Nanjing, 210093, China
2. Department of Geography of Sun Yat-sen University, Guangzhou, 510275, China
3. Construction Bureau of Zhejiang Province, Hangzhou, 310027, China
4. Department of Humanities and Social Sciences of Bengbu College, Bengbu, 233050, Anhui, China
5. Department of Geography of Chuzhou University, Chuzhou, 239012, Anhui, China
6. Management Committee of Scenic Areas in Fangyan, Yongkang City of Zhejiang Province, Yongkang, 321308, Zhejiang, China
7. College of Urban and Environmental Sciences of Peking University, Beijing, 100871, China - ISSN：1861-9568
文摘
The prominent types of Danxia landform in Fangyan include enclosed valleys, mesas, peaks, stone columns and grooves etc. Their spatial combinations have regular configurations along the northwest-southeast direction: typical grooves and caves are located in the northwestern Wufengshuyuan mainly; abundant fresh collapsed stones may be observed in central Jimingfeng and Taohuafeng; stone drums and stone columns are in the southeastern Shiguliao particularly; enclosed valleys are encircling joints of peaks and plains from three directions east, west, and south. Their spatial combinations reflect that the developments of Danxia landform have undergone stages of geomorphic cyclical erosion in the form of weathering, collapse, transportation, sedimentation and other processes, together with the “sculpture-of external forces mainly as tectonic uplift. The picturesque Danxia landform began its formation at that point. Danxia landform developed mainly in the strata of Fangyan Formation (K1 f) caused by the alluvial fan-braided river phase of anterior fan in the late period of the Early Cretaceous. Regular patterns of weathering of stones and features of braided alluvial phase sediments may be verified by the analysis of three groups of experimental data. Danxia landform of Fangyan is a unique representative of the “adolescent-development type in the application of the World Natural Heritages status in China, by virtue of its outstanding universal aesthetic and scientific value.