ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
山东岩溶地貌特征及其形成演化分析
投稿时间:2020-02-05  修订日期:2020-03-22
关键词:Spring  Gu  Discrete Island  Karst Landform of Temperate Zone  Shandong Karst
基金项目:
作者单位E-mail
韦跃龙 中国地质科学院岩溶地质研究所 weiyuelong@karst.ac.cn 
摘要点击次数: 82
全文下载次数: 0
摘要:
Characteristics and Formation and Evolution Analysisof the Karst Landforms of Shandong
      The karst landforms in Shandong are generally classified into the karst landforms that have Shandong characteristics, including Gu group, coast etc, and the typical karst landforms that develop in north China and temperate zone, including spring group, long wall shape mountain, dry valley etc, and the karst landforms that often have been seen, including cave group,doline, depression, gorge etc. All of them have been developed in the soluble stratum that is dominated by the Cambrian and the Ordovician. They appeared to be linear–like,or planar-like,or point-like and distributed in numerous karst islands which have different scales and shapes and are completely independent of each other. They are a typical concentration of Gu group, spring group, cave group and coast, and are one of the most typical representative for presenting Gu and spring. Based on the analysis and investigation about the regional geological and geographical background, Shandong karst landforms is divided into 3 karst landform regions of warm temperate zone(including semiarid, semihumid and coast)according to the characteristics of regional climate, then this paper systematically studies and discusses the formation and evolution of discrete island of Shandong karst, and hold that it is the typical representative place that couldSfullySdisplaySthe
  查看/发表评论  下载PDF阅读器
Copyright©2008 《地球学报》编辑部 All Rights Reserved
Sponsored by:中华人民共和国自然资源部
Address:: 北京市西城区百万庄大街26号,中国地质科学院东楼317室 PostCode:100037 Tel:010-68327396 E-mail: diqiuxb@126.com