[1]齐德利,颜 明,闫 丹,等.中国丹霞地貌的面积概算——粤北坪石红层盆地的实证研究[J].山地学报,2016,(02):134-141.[doi:10.16089/j.cnki.1008-2786.000110]
　QI Deli,YAN Ming,YAN Dan,et al.Estimate Area of Danxia Landform in China ——an empirical research on Pingshi Red-beds Basin in Northern Guangdong[J].Mountain Research,2016,(02):134-141.[doi:10.16089/j.cnki.1008-2786.000110]
点击复制

中国丹霞地貌的面积概算——粤北坪石红层盆地的实证研究()
分享到：

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年02期
页码:
134-141
栏目:
山地生态与环境
出版日期:
2016-04-01

文章信息/Info

Title:
Estimate Area of Danxia Landform in China ——an empirical research on Pingshi Red-beds Basin in Northern Guangdong
作者:
齐德利; 颜 明; 闫 丹; 李炳元
中国科学院地理科学与资源研究所地貌研究室,北京 100101
Author(s):
QI Deli; YAN Ming; YAN Dan; LI Bingyuan
Institute of Geographic Sciences and Natural Resources of Research, CAS, Beijing, 100101, China
关键词:
丹霞地貌;  红层盆地;  面积;  中国
Keywords:
Danxia landform;  red beds basin;  landscape contribution rate;  area;  Pingshi;  China
分类号:
P931
DOI:
10.16089/j.cnki.1008-2786.000110
文献标志码:
A
摘要:
中国丹霞地貌的中生代优势以及陆相沉积特征是中国的特色也具有世界代表性。通过对中生代主要出露红层盆地室内计算机空间叠置分析,利用大量的野外现场调研检验等手段,计算出不同时期不同规模的红层面积。其中,中侏罗世3个红盆面积45.16×104 km2,中、晚侏罗世28个红盆面积149.17×104,早白垩世17个红盆面积55.97×104 km2,晚白垩世24个红盆面积106.9×104 km2,早第三纪31个红盆面积135.73×104 km2。通过对实地测量及对比分析,发现红层盆地建造发育成丹霞地貌的贡献率为6.5%左右。可计算中、晚侏罗世红层发育的丹霞地貌面积为9.7×104 km2,早白垩世红层发育的丹霞地貌面积3.6×104 km2,晚白垩世24个红盆面积6.9×104 km2,早第三纪31个红盆面积8.8×104 km2,这样统计中国丹霞地貌的总面积为29×104 km2。这一数字因丹霞地貌自身发育的阶段性会出现偏差,考虑气候-构造-地貌相互耦合作用的结果,典型丹霞地貌随着时间的推移,增加和减少的面积将达到一个平衡,基本稳定在20×104 km2左右,这就是中国丹霞地貌的面积数据。
Abstract:
It is very representative in the world that Danxia Landform in China with mainly formed from Mesozoic layers, such as red-coloured sandstones and conglomerates so on, which almost from continental sedimentary feature. Based on spatial overlay analysis, compared with field survey test, firstly this paper calculated the area of red beds in different periods and different sizes. Three red basins in the Middle Jurassic an area of 45.16×104 km2, 28 red basin in middle and late Jurassic of 149.17×104 km2, 17 red basins in early Cretaceous of 55.97×104 km2, 24 red basins in Late Cretaceous of 106.9×104 km2, and 31 red basins in early third century of 135.73×104 km2. Through analysis of field measurement and comparison form Pingshi Red-beds basin, the landscape contribution rate is about 6.5%, from red beds to Danxia landform. So the total area of Danxia landform of China is about 32×104 km2. Consider the climatic and tectonic and landform interaction results, during the Danxia landform development stage of the deviation, the area of classical Danxia landform will reach a balance and maintained at 20×104 km2. It is the basic area data of Danxia landform in China.

参考文献/References:

[1] Kuota Chan. On the Subdivisions of the Red Beds of South-Eastern China[J].Bulletin of the Geological Society of China,1939,18(3/4):301-321
[2] 黄进,陈致均.丹霞地貌定义及分类中一些问题的探讨[J].经济地理,2003,23(增刊):6-11[Huang Jin, Chen Zhijun. The Discussion on the Definition and Classification to Danxia Landform[J]. Economic Geography, 2003,23(suppl.):6-11]
[3] 黄进,陈致均,齐德利.中国丹霞地貌分布(上)[J]. 山地学报,2015,23(4):385-396[Huang Jin, Chen Zhijun, Qi Deli.Study on Distribution of Danxia Landform in China(First)[J].Mountain Research, 2015,23(4):385-396]
[4] 黄进,陈致均,齐德利.中国丹霞地貌分布(下)[J]. 山地学报,2015,23(6):640-648[Huang Jin, Chen Zhijun, Qi Deli.Study on Distribution of Danxia Landform in China(Last)[J].Mountain Research, 2015,23(6):640-648]
[5] 理查德.哈特向著.叶光庭译.地理学的性质[M].北京:商务印书馆,1996:508,47[Richard Hartshorne. The Nature of Geography: A Critical Survey of Current Thought in the Light of the Past[M].Beijing: The Commercial Press.1996: 508,47]
[6] 大卫.哈维著.高泳源,刘立华,蔡运龙译.地理学中的解释[M].北京:商务印书馆,1996:507[David Harvey.Explanation in Geography [M]. Beijing: the Commercial Press, 1996:507]
[7] 齐德利,肖星,陈致均.甘肃省丹霞地貌空间分析及旅游开发布局研究[J].地理与地理信息科学,2003,19(3):88-93[Qi Deli, Xiao Xing, Chen Zhijun. Spatial analysis and tourism developmental layout on Danxia landscape in Gansu Province[J].Geography and Geo-Information Science,2003,19(3):88-93]
[8] Qi Deli, Yu Rong, Zhang Renshun, et al. Comparison study on Danxia landform in China[J]. Journals of Geographical Sciences, 2005,15(3):337-345
[9] 杨志,郭福生,刘林清.基于MapGIS的江西省丹霞地貌信息系统设计与开发[J].测绘与空间地理信息,2006,29(1):64-66[Yang Zhi, Guo Fusheng, Liu Linqing. Research and realization of Danxia landform information system of Jiangxi Province Based on MapGIS[J]. Geomantic & Spatial Information Technology, 2006,29(1):64-66]
[10] 彭华.中国红石公园-丹霞山[M].北京:地质出版社,2004:1-120[Peng Hua. Danxiashan-The red stone park of China [M]. Beijing: Geological Publishing House,2004:1-120]
[11] 俞锦标,杨剑明,王祥,申屏.构造盆地与丹霞地貌[J].经济地理(增刊),1996:115-121[Yu Jinbiao, Yang Jianming, Wang Xiang, Shen Ping. Tectonic Basins and Danxia Landforms[J]. Economic Geography,1994,14(suppl.):115-121]
[12] 童亨茂,曹代勇,秦红.中国沉积盆地复杂性的表现形式及其成因剖析[J].地质力学学报,2004,10(2):146-154[Tong Hengmao,Cao Daiyong,Qin Hong.Complexity causes explanation and characteristics analysis of oil and gas distribution in the sedimentary basins of China[J].Journal of Geomechanics,2004,10(2):146-154]
[13] 程裕淇.中国区域地质概论[M].北京:地质出版社,1994:461-466; 474-475[Chen Yuqi.Regional Geology of China[M].Beijing: Geological Publishing House,1994:461-466; 474-475]
[14] 宋青春,杨振春.地质学基础[M].北京:高等教育出版社,1996:355[Song Qingchun, Yang Zhenchun. Basic Geology [M]. Beijing: Higher Education Press, 1996:355]
[15] 王鸿祯.中国古地理图集[M].北京:地图出版社,1985: 97-142[Wang Hongzhen. Atlas of the palaeogeography of China[M]. Beijing: Cartographic Publishing House,1985: 97-142]
[16] 中国地质科学院.中国地层1-中国地层概论[M]. 北京:地质出版社,1982.[Chinese Academy of Geological Sciences. Stratigraphy of China(No.1):An Outline of the Stratigraphy in China[M]. Beijing: Geological Publishing House,1982.]
[17] 王思恩,程政武,王乃文,等.中国地层11-中国的侏罗系[M].北京:地质出版社,1985:1-332[Wang Sien, Cheng Zhengwu, Wang Naiwen,et al. Chinese Strata(No.11):The Jurassic of China[M]. Beijing: Geological Publishing House, 1985:1-332]
[18] Hao Yichun, Su Deying, Yu Jingxian,et al. Chinese Strata(No.12):The Cretaceous of China[M]. Beijing: Geological Publishing House, 1986:1-284[郝诒纯,苏德英,余静贤,等.中国地层12-中国的白垩系[M].北京:地质出版社,1986:1-284]

相似文献/References:

[1]姜勇彪,郭福生,陈珊珊,等.江西信江盆地丹霞地貌空间分布及其成因[J].山地学报,2013,(06):731.
　JIANG Yongbiao,GUO Fusheng,CHEN Shanshan.Spatial Distribution and Its Genesis of the Danxia Landforms in Xinjiang Basin, Jiangxi[J].Mountain Research,2013,(02):731.
[2]郭福生,姜伏伟,胡中华,等.丹霞地貌危岩景观分类及可持续开发对策——以龙虎山景区为例[J].山地学报,2012,(01):99.
　GUO Fusheng,JIANG Fuwei,HU Zhonghua,et al.Danxia Landscape Rockfalllandscape Types and Protection Measures—— A Case Study of Mt. Longhushan in Jiangxi, China[J].Mountain Research,2012,(02):99.
[3]郭福生,姜勇彪,胡中华,等.龙虎山世界地质公园丹霞地貌成景系统特征及其演化[J].山地学报,2011,(02):195.
　GUO Fusheng,JIANG Yongbiao,HU Zhonghua,et al.Evolution and Genesis System Features of Danxia Lanform in Longhushan World Geopark[J].Mountain Research,2011,(02):195.
[4]周学军.中国丹霞地貌的南北差异及其旅游价值[J].山地学报,2003,(02):180.
[5]姜勇彪,郭福生,孙传敏,等.江西弋阳县龟峰丹霞地貌景观特征与形成机制[J].山地学报,2008,(01):120.
[6]姜勇彪,郭福生,胡中华,等.龙虎山世界地质公园丹霞地貌特征及与国内其他丹霞地貌的对比[J].山地学报,2009,(03):353.
[7]张广胜,朱诚,俞锦标,等.浙江江郎山丹霞地貌区岩性特征[J].山地学报,2010,(03):301.
[8]黄宝华,郭福生,姜勇彪,等.广丰盆地丹霞地貌遥感影像特征[J].山地学报,2010,(04):500.
[9]姜勇彪,郭福生,胡中华,等.信江盆地丹霞地貌特征及其景观类型[J].山地学报,2010,(04):505.
[10]嘉益.封面照片:丹霞山[J].山地学报,2015,(03):293.

备注/Memo

备注/Memo:
收稿日期(Received date):2015-08-31; 改回日期(Accepted): 2015-12-01。 基金项目(Foundation item):国家自然科学基金项目( No.41371035)和国家科技基础性工作专项( No.2013FY111900)。[ Project supported by the National Nature Science Foundation of China( No.41371035 )and Basic work of the National Science and Technology Special Fund( No.2013FY1119000).] 作者简介(Biography):齐德利(1973-),男,宁夏隆德人,博士。研究方向为丹霞地貌。[Qi Deli(1973-), male, born in Ningxia, Doctor and mainly study on Danxia Landform. ]E-mail: qidl@igsnrr.ac.cn
更新日期/Last Update: 1900-01-01