[1]王世杰,张信宝,白晓永.中国南方喀斯特地貌分区纲要[J].山地学报,2015,(06):641-648.[doi:10.16089/j.cnki.1008-2786.000079]
 WANG Shijie,ZHANG Xinbao,BAI Xiaoyong.An Outline of Karst Geomorphology Zoning in the Karst Areas of Southern China[J].Mountain Research,2015,(06):641-648.[doi:10.16089/j.cnki.1008-2786.000079]
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中国南方喀斯特地貌分区纲要()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年06期
页码:
641-648
栏目:
学科前言及热点
出版日期:
2015-12-01

文章信息/Info

Title:
An Outline of Karst Geomorphology Zoning in the Karst Areas of Southern China
作者:
王世杰13张信宝23白晓永13
1. 中国科学院地球化学研究所/环境地球化学国家重点实验室, 贵州 贵阳 550002; 2. 中国科学院水利部成都山地灾害与环境研究所, 四川 成都 610041; 3. 中国科学院普定喀斯特生态系统观测研究站, 贵州 普定 562100
Author(s):
WANG Shijie13 ZHANG Xinbao23 BAI Xiaoyong13
1. State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry, Chinese Academy of Sciences,Guiyang 550002,Guizhou,China; 2.Institute of Mountain and Environment,Chinese Academy of Sciences,Chengdu 610041,Sichuan,China; 3. Karst Ecosystem Observation Research Station in Puding,Chinese Academy of Sciences,Puding 562100,Guizhou,China
关键词:
中国南方 喀斯特 地貌分区 纲要
Keywords:
Southern China karst geomorphology Zoning outline
分类号:
P931.5
DOI:
10.16089/j.cnki.1008-2786.000079
文献标志码:
A
摘要:
对热带喀斯特地貌形成的动力学机制和任美锷先生提出的喀斯特地貌演化理论展开讨论,并遵循地貌类型的地带性和非地带性规律,根据地貌形态和成因的相似性,提出我国南方喀斯特地貌分区纲要。根据喀斯特地貌的气候类型,南方喀斯特地区分为:热带喀斯特地貌类型区和非热带喀斯特地貌类型区。根据喀斯特地貌形态组合,热带喀斯特地貌类型区再分为:黔中高原浅碟型峰丛洼地,黔-桂斜坡带漏斗型峰丛洼地和广西峰林平原等3个亚区。根据区域地貌形态,非热带喀斯特地貌类型区再分为:川西、滇西北中高山,滇东高原盆谷,北盘江高原峡谷,黔渝川鄂湘接壤的中低山槽谷,湘中、湘南、鄂东中低山丘陵区等5个亚区。
Abstract:
Dynamic mechanism for formation of trdopical karst geomorphology and karst geomorphology evolution, proposed by Prof. Ren mei'e, are discussed in this paper. Based on zonality and anonality laws of geomorphology types and according to similarities of the karst geomorphology and its formation causes, an outline of karst geomorphology zoning in the karst areas of Southern China is proposed. According to climate types of the karst geomorphology, the areas are divided into tropical karst geomorphology zone and non-tropical karst geomorphology zone. According to karst morphology group, the tropical karst geomorphology zone is divided into the Peak-Cluster Depression subzone of shallow dish type in the middle Guizhou Plateau; the Peak-Cluster Depression subzone of funnel type in the transition slope between Guizhou Plateau and Gaunxi Hilly plain. According to regional geomorphology, the non-tropical karst geomorphology zone is divided into the medium-high mountain subzone in Western Sichuan and North-western Yunnan; the basin-valley subzone in Eastern Yunnan Plateau; the canyon subzone of Beipan River; the trough valley subzone of the medium-low mountains in the conjunction region between Guizhou, Chongqing, Sichuan, Hubei and Hunan; and the non-trough valley subzone of the medium-low mountains and hills in Middle and Southern Hunan and Eastern Hubei.

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备注/Memo

备注/Memo:
收稿日期(Received date):2015-08-11; 修回日期(Accepted):2015-09-23。 基金项目(Foundation item):国家973项目( No.2013CB956704),国家科技支撑计划(No.2014BAB03B02),贵州省科技计划( No.黔科合重大专项字﹝2012﹞6015号),贵州省农业攻关计划项目(No.黔科合NY字〔2014〕3039号),贵阳市科技局项目(No.筑合同[2012205]号),“西部之光”之西部博士专项(No.科发人教字〔2012〕179 号)。 作者简介(Biography):王世杰(1966-),男,研究员,博士生导师,主要从事喀斯特生态环境研究。[Wang Shijie(1966- ), male, professor, doctoral supervisor, specialized in karst environment.] E-mail: wangshijie@vip.Skleg.cn
更新日期/Last Update: 1900-01-01