Advanced Search
  • Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 40 Issue 5
Oct.  2021
Turn off MathJax
Article Contents
Article Navigation >  CARSOLOGICA SINICA  > 2021  >  40(5): 750-759
LUO Shuwen,HE Wei,YANG Tao,et al.Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor[J].Carsologica Sinica,2021,40(05):750-759. doi: 10.11932/karst20210502
Citation: LUO Shuwen,HE Wei,YANG Tao,et al.Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor[J].Carsologica Sinica,2021,40(05):750-759. doi: 10.11932/karst20210502
shu

Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor

doi: 10.11932/karst20210502
  • 1.

    Guizhou Institute of Mountain Resources Research，Guiyang， Guizhou 55001， China

  • 2.

    Institute of Karst Geology，CAGS，Guilin，Guangxi 541004， China

  • 3.

    Guiyang No.12 Middle School ， Guiyang，Guizhou 550002， China

  • 4.

    Key Laboratory of Karst Dynamics，MNR & GZAR， Guilin，Guangxi 50002，China

Funds:

 2016YFC0502606

 [2017]5720

 [2016]21

 [2019]08

 DD20190022

  • Received Date: 2021-03-30
  • Publish Date: 2021-10-25
    Abstract
  • To explore the karst development characteristics， hydrogeomorphological significance and the causes of formation of peak forest plain in Hunan-Guangxi Corridor，in this paper，the investigation of spatial distribution characteristics of landforms， lithology and landform types in the area are conducted ，and the formation and evolution of  hydrogeomorphology are discussed under the guidance of karst hydrogeomorphology theory.The analysis of the spatial distribution characteristics  shows that the water system in this area has undergone a reverse seizure process； its regional geomorphic evolution is affected by the uplift of Yuechengling and Haiyangshan mountains， which has led to the narrowing of the Hunan-Guangxi Corridor and diversion of the Xiangjiang river to northeast. The geomorphic evolution has experienced at least three flattening periods， the ancient Xiangjiang period，the Linghe incubation period， and the Linghe period. In addition，the concept model of the karst basin intertidal zone as well as the interactive capture mode of karst basin are put forward for the first time when the formation dynamic mechanism of peak forest plain is analyzed， which enriches the genetic type of peak forest plain and the research methods of karst hydrogeomorphology. The scientific terms put forward here is also of  important scientific implications.

     

    • LUO Shuwen,HE Wei,YANG Tao,et al.Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor[J].Carsologica Sinica,2021,40(05):750-759.
    FullText(HTML)
  • loading
    • References(24)
  • 任美锷，刘振中，王飞燕，等.岩溶学概论［M］.北京：商务印出馆，1983.4.
    FordDerek ， WilliawsPaul. Karst Hydrogeolgy and Geomorphology［M］. London： UnwinHyman， 2007.
    朱学稳，汪训一，朱德浩，等.桂林岩溶地貌与洞穴研究［M］.北京：地质出版社，1988.
    袁道先，蔡桂鸿.岩溶环境学［M］.重庆：重庆出版社，1988.
    MylroieJ E. Hydrologic classification of cavesandkarst［M］. In：Groundwater asageomorphicagent， editedby： R G， LaFleur， Allen & Unwin，Inc.， Boston， MA，1984：157-172.
    BogliA. Karst hydrology and speleology［M］.Berlin：Springer，1980.
    朱学稳.峰林喀斯特的性质及其发育和演化的新思考（1）［J］.中国岩溶，1991，10（1）：51-62.
    朱学稳.峰林喀斯特的性质及其发育和演化的新思考（2）［J］.中国岩溶，1991，10（2）：137-149.
    朱学稳.峰林喀斯特的性质及其发育和演化的新思考（3）［J］.中国岩溶，1991，10（3）：171-182.
    P WWilliamset al . Geomorphic inheritance and the development of tower karst ［J］. Earth Surface Processes and Land formsG， 1987， 12（ 5）： 453-465.
    罗书文，陈伟海，黄保健，等.贵州喀斯特流域水文地貌系统演化［A］//全国第十五届洞穴学术会议暨乐业·凤山地质公园发展研讨会议论义选集［C］.北京：地质出版社，2012.
    杨明德，谭明，梁虹.喀斯特流域水文地貌系统［M］.北京：地质出版社，1998.
    谭明.喀斯特水文地貌学——理论、方法及应用研究［M］.贵阳：贵州人民出版社，1993.
    王元林.隋唐五代时期岭南海陆丝路变迁与苍梧郡地位的变化［J］.广西名族大学学报（哲学社会科学版），2017，39（1）：66-72.
    JakucsL. Morphogenetics of karst regions［M］.Hilger，1977：54.
    曾昭璇.岩石地形学［M］.北京：地质出版社，1960.
    曾昭璇.论我国南部喀斯特地形的特征［J］.中国岩溶，1982，1（1）：27-32.
    焦树林，梁虹.喀斯特地区流域地貌与岩性的统计关系探讨：以贵州省为例［J］.中国岩溶，2002，21（2）：95-100.
    张之淦.岩溶发生学——理论探索［M］.桂林：广西师范大学出版社，2006，12.
    张美良，刘功余，邓自强，等.广西白垩世古岩溶与成矿研究［M］.北京：地质出版社，2010.
    易连兴，夏日元，王喆，等.岩溶地下河探测与评价［M］.北京：地质出版社，2018.
    罗书文，杨桃，潘晓东，等.贵州落脚河峡谷景观特征及形成机制［J］.重庆师范大学学报（自然科学版），2019，36（4）：112-121.
    罗书文，邓亚东，黄保健，等.广西田东棋盘滩地质奇观的形成机理［J］.华南师范大学学报（自然科学版），2016，48（4）：71-76.
    广西壮族自治区地质矿产局.广西壮族自治区区域地质志［M］.北京：地质出版社，1987.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Get Citation
    PDF(1569.0KB)
    XML

    Article Metrics

    Article views (1376) PDF downloads(78) Cited by()
    Proportional views
    Related

    Website Copyright © CARSOLOGICA SINICA 桂ICP备05009877号-1

    Sponsor: Chinese Academy of Geological Sciences Sponsored by: Institute of Karst Geology, Chinese Academy of Geological Sciences Address: No.50, Qixing Road, Guilin, Guangxi

    Post Code: 541004 Tel: 0773-5812949 7796657 Email: zgyr@mail.cgs.gov.cn; zgyrbjb@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd.    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return