浙江方岩丹霞地貌类型及其空间组合

doi:10.11821/xb200903010

地理学报 ›› 2009, Vol. 64 ›› Issue (3): 349-356.doi: 10.11821/xb200903010

浙江方岩丹霞地貌类型及其空间组合

欧阳杰¹, 朱诚¹, 彭华², 俞锦标¹, 李兰¹, 周日良³, 张广胜¹, 朱光耀⁴, 李中轩¹, 钟宜顺⁵, 朱青¹, 吕文¹, 胡永起⁶, 郑朝贵⁵, 吕振荣⁶, 胡昶⁶, 武弘麟⁷

1. 南京大学地理与海洋科学学院,南京210093;
2. 中山大学地理系,广州510275;
3. 浙江省建设厅,杭州310027;
4. 安徽蚌埠学院人文与社会科学部,安徽蚌埠233050;
5. 安徽滁州学院地理系,安徽滁州239012;
6. 浙江永康市方岩风景名胜区管理委员会,浙江永康321308;
7. 北京大学城市与环境学院,北京100871

收稿日期:2008-11-03 修回日期:2009-01-06 出版日期:2009-03-25 发布日期:2009-03-25
通讯作者: 朱诚,教授,博士生导师,E-mail: zhuchengnj@yahoo.com.cn
作者简介:欧阳杰,博士研究生,自然地理与第四纪地质学专业。E-mail: oyang692000@yahoo.com.cn
基金资助:
国家自然科学基金资助项目(40871014);浙江省建设厅申报世界遗产项目和南京大学现代分析中心测试基金资助

Types and Spatial Combination of Danxia Landforms of Fangyan in Zhejiang Province

OUYANG Jie¹, ZHU Cheng¹, PENG Hua², YU Jinbiao¹, LI Lan¹, ZHOU Riliang³, ZHANG Guangsheng¹, ZHU Guangyao⁴, LI Zhongxuan¹, ZHONG Yishun⁵, ZHU Qing¹, Lv Wen¹, HU Yongqi⁶, ZHENG Chaogui⁵, Lv Zhenrong⁶, HU Chang⁶, WU Honglin⁷

1. School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,China;
2. Department of Geography,Sun Yat-sen University,Guangzhou 510275,China;
3. Zhejiang Construction Bureau,Hangzhou 310027,China;
4. Department of Humanities and Social Sciences,Bengbu College,Bengbu 233050,Anhui,China;
5. Department of Geography,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,Peking University,Beijing 100871,China

Received:2008-11-03 Revised:2009-01-06 Online:2009-03-25 Published:2009-03-25
Supported by:
National Natural Science Foundation,No.40871014;Project of Application International Natural Heritages of Construction Bureau of Zhejiang Province;The Test Foundation of Modern Analyses Center of Nanjing University

摘要/Abstract

摘要：

浙江方岩突出的丹霞地貌类型有围谷、方山、峰丛、石柱和凹槽等，它们的空间组合沿着北西—南东方向有规律的排列：西北部五峰书院一带的凹槽和岩穴发育典型，中部鸡鸣峰、桃花峰等处分布有大量的新鲜崩积石，东南部石鼓寮的石鼓、石柱尤为突出，在峰丛与平原交汇的东、南和西三侧被围谷所环绕。这种组合体现了随着构造隆升，在以外力作用为主的不断“雕塑” 下，丹霞地貌的发育一般经历了差异风化、重力崩塌、流水侵蚀搬运，完成地貌循环侵蚀的过程，期间孕育了绚丽多姿的丹霞地貌，它们主要发育于早白垩世晚期的方岩组(K1f) 冲积扇—扇前辫状河相岩层中。其中，岩性的差异风化规律和辫状河相沉积的特点，可以通过对三个样点的实验数据分析加以证实。方岩丹霞地貌是在我国申报世界自然遗产丹霞地貌区中“青年期” 类型的突出代表，符合申报世界自然遗产中具有突出、普遍的美学和科学价值的理由。

关键词: 浙江方岩, 丹霞地貌, 方岩组

Abstract:

The prominent types of Danxia landform in Fangyan include enclosed valleys, mesas, peaks, stone columns and grooves etc. Their spatial combination has regular order along the direction of northwest-southeast: typical grooves and caves are mainly located in northwestern Wufengshuyuan; abundant fresh collapsed stones can 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 of east, west, and south. The spatial combination suggests that the development of Danxia landform experienced procedures of geomorphic cycle erosion of weathering, collapse, erosion by rivers etc. under the "sculpture" of external force mainly as tectonic uplifting, picturesque Danxia landform was conceived then. They are developed mainly in the strata of Fangyan Formation (K1f) of alluvial fan-braided river phase of anterior fan in the late period of Early Cretaceous. Regular pattern of weathering of stones and features of sediments of braided river phase can be identified by analysis of experimental data obtained from three sample points. Danxia landform of Fangyan is a unique representive of the "adolescent" type of China's Danxia landform in the application of the World Natural Heritages with outstanding universal aesthetic and scientific value.

Key words: Fangyan of Zhejiang Province, Danxia landform, Fangyan Formation

欧阳杰,朱诚,彭华,俞锦标,李兰,周日良,张广胜,朱光耀,李中轩,钟宜顺,朱青,吕文,胡永起,郑朝贵,吕振荣,胡昶,武弘麟. 浙江方岩丹霞地貌类型及其空间组合[J]. 地理学报, 2009, 64(3): 349-356.

OUYANG Jie,ZHU Cheng,PENG Hua,YU Jinbiao,LI Lan,ZHOU Riliang,ZHANG Guangsheng,ZHU Guangyao,LI Zhongxuan,ZHONG Yishun,ZHU Qing,Lv Wen,HU Yongqi,ZHENG Chaogui,Lv Zhenrong,HU Chang,WU Honglin. Types and Spatial Combination of Danxia Landforms of Fangyan in Zhejiang Province[J]. Acta Geographica Sinica, 2009, 64(3): 349-356.

参考文献

[1] Chen Chuankang, Gao Yugong, Yu Kongjian et al. A study on tourism development of the Danxia scenic district. Acta Geographica Sinica, 1990, 45(3): 284-294.
[陈传康, 高豫功, 俞孔坚等. 丹霞风景名胜区的旅游开发研究. 地理学报. 1990, 45(3): 284-294.]

[2] Peng Hua. A survey of the Danxia landform research in China. Scientia Geographica Sinica, 2000, 20(3): 203-211.
[彭华. 中国丹霞地貌研究进展. 地理科学, 2000, 20(3): 203-211.]

[3] Zhou Xuejun. A study on north-south differences of the Danxia landform pattern and its tourism values in China. Journal of Mountain Science, 2003, 21(2): 180-186.
[周学军. 中国丹霞地貌的南北差异及其旅游价值. 山地学报, 2003, 21(2): 180-186.]

[4] Qi Deli, Yu Rong, Zhang Renshun et al. On the spatial pattern of Danxia landform in China. Acta Geographica Sinica, 2005, 60(1): 41-52.
[齐德利, 于蓉, 张忍顺等. 中国丹霞地貌空间格局. 地理学报, 2005, 60(1): 41-52.]

[5] Luo Hao, Chen Jingtang, Zhong Guoping. A comparison between the tourism scenery of Danxia landform and that of karst landform. Tropical Geography, 2006, 26(1): 12-17.
[罗浩, 陈敬堂, 钟国平. 丹霞地貌与岩溶地貌旅游景观之比较研究. 热带地理, 2006, 26(1): 12-17.]

[6] Chen Liangwen. The vantage of touristry resource of Danxia landform scenery region in Zhejiang Province. Journal of Zhejiang University (Sciences Edition), 2000, 27(5): 564-567.
[陈谅闻. 浙江丹霞地貌风景区的旅游资源优势. 浙江大学学报(理学版), 2000, 27(5): 564-567.]

[7] Lu Huijin. Danxia landform and its tourism resource in the mid-western area of Zhejiang Province. Geology of Zhejiang, 2001, 17(2): 66-73.
[吕惠进. 浙江省中西部地区丹霞地貌特征及其旅游资源. 浙江地质, 2001, 17(2): 66-73.]

[8] Huang Jin. A kind of basic mode of slope development of Danxia landform. Tropical Geomorphology, 1982, 3 (2): 107-134.
[黄进. 丹霞地貌剖面发育的一种基本方式. 热带地理, 1982, 3(2): 107-134.]

[9] Zhu Cheng, Yu Jinbiao, Li Gang et al. Danxia landform genesis and scenic feature on Guanzai Mountain, Fujian Province. Acta Geographica Sinica, 2000, 55(6): 679-688.
[朱诚, 俞锦标, 李刚等. 福建冠豸山丹霞地貌成因及旅游景观特色. 地理学报, 2000, 55(6): 679-688.]

[10] Zhu Cheng, Peng Hua, Li Shicheng et al. Danxia landform genesis on Qiyun Mountain, Anhui Province. Acta Geographica Sinica, 2005, 60(3): 445-455.
[朱诚, 彭华, 李世成等. 安徽齐云山丹霞地貌成因. 地理学报, 2005, 60 (3): 445-455.]

[11] Ministry of Geology and Mineral Resources of People's Republic of China, Bureau of Geology and Mineral Resources of Zhejiang Province. Regional Geological Records of Zhejiang Province. Beijing: Geological Publishing House, 1989.
[中华人民共和国地质矿产部, 浙江省地质矿产局. 浙江省区域地质志. 北京: 地质出版社, 1989.]

[12] Zeng Zhaoxuan, Huang Shaomin. Red bed in southeastern China. Journal of South China Normal University (Natural Science), 1978, (2): 43-57.
[曾昭璇, 黄少敏. 中国东南部红层地貌. 华南师范学院学报(自然科学版), 1978, (2): 43-57.]

[13] Peng Hua, Wu Zhicai. A preliminary study on the characteristics and the distribution of red beds. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2003, 42(5): 109-113.
[彭华, 吴志才. 关于红层特点及分布规律的初步探讨, 中山大学学报, 2003, 42(5): 109-113.]

[14] Office of Geology and Mineral Resources of Zhejiang Province. Specification of Geological map of the People's Republic of China-Breadth of Yongkang (H-51-109-A). Hangzhou: Printing plant of map of regional geological survey group of Zhejiang province, 1995. 1-15.
[ 浙江省地质矿产厅. 中华人民共和国地质图说明书: 永康市幅 (H-51-109-A). 杭州: 浙江省区域地质调查大队制图印刷厂, 1995. 1-15.]

浙江方岩丹霞地貌类型及其空间组合

Types and Spatial Combination of Danxia Landforms of Fangyan in Zhejiang Province

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 6

Metrics

本文评价

[1]	彭华, 潘志新, 闫罗彬, Scott SIMONSON. 国内外红层与丹霞地貌研究述评[J]. 地理学报, 2013, 68(9): 1170-1181.
[2]	朱诚,彭华,李中轩,俞锦标,李兰,张广胜,朱光耀,欧阳杰,钟宜顺,朱青,周书勤,郑朝贵,周日良,李东,朱雨鸣,吕文,武弘麟. 浙江江郎山丹霞地貌发育的年代与成因[J]. 地理学报, 2009, 64(1): 21-32.
[3]	朱诚, 彭华, 李世成, 黄林燕, 郑朝贵, 项伏生,孙毓飞, 唐云松, 胡济源, 朱光辉, 吕健君, 程光华. 安徽齐云山丹霞地貌成因[J]. 地理学报, 2005, 60(3): 445-455.
[4]	齐德利, 于蓉, 张忍顺, 葛云健, 李加林. 中国丹霞地貌空间格局[J]. 地理学报, 2005, 60(1): 41-52.
[5]	朱诚, 俞锦标, 赵宁曦, 李刚, 吴承照. 福建冠豸山丹霞地貌成因及旅游景观特色[J]. 地理学报, 2000, 55(6): 679-688.
[6]	陈传康, 高豫功, 俞孔坚, 彭华 . 丹霞风景名胜区的旅游开发研究 [J]. 地理学报, 1990, 45(3): 284-294.