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Volume 39 Issue 1
Feb.  2020
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Article Navigation >  CARSOLOGICA SINICA  > 2020  >  39(1): 119-126
WU Jin, ZHANG Zhaohui. Research status and prospect of karst Tiankengs in Guizhou Province[J]. CARSOLOGICA SINICA, 2020, 39(1): 119-126. doi: 10.11932/karst2019y35
Citation: WU Jin, ZHANG Zhaohui. Research status and prospect of karst Tiankengs in Guizhou Province[J]. CARSOLOGICA SINICA, 2020, 39(1): 119-126. doi: 10.11932/karst2019y35
shu

Research status and prospect of karst Tiankengs in Guizhou Province

doi: 10.11932/karst2019y35

  • Key Laboratory for Information System of Mountainous Area and Protection of Ecological Environment of Guizhou Province, Guizhou Normal University, Guiyang，Guizhou 550001，China

  • Publish Date: 2020-02-25
    Abstract
  • Guizhou Province is located in the southwest of China, east of the Yunnan-Guizhou Plateau, topographically high in the west and low in the east. It is near the southeast continental margin, part of the upstream ecotone of the Yangtze River and the Pearl River. It is an important ecological barrier for the upstream areas of the Yangtze River and the Pearl River. This region hosts typical karst landforms which are widely distributed and of various types, and geographically distinct. Karst carbonate rocks are dominant where karst Tiankeng developed well. Karst Tiankeng is a negative geomorphology, widely present in central, northwest and southern Guizhou Province, China. It is characterized by large number, wide distribution and strong stability of inner environments. Based on the special geomorphology and topography of Guizhou, combined with research reports of karst Tiankeng availlable, this work conducted field investigations and statistical analysis of literature data on this phenomenon. The purpose is to review the research status of the geological background, origin, types and distribution patterns of karst Tiankeng in Guizhou, and puts forward the prospect of its development trend and research direction. The results show that， (1) There are 25 karst sinkholes in total in Guizhou. According to the depth, shape and scale, they are categorized into 3 super sinkholes, 2 large sinkholes, 18 medium sinkholes and 2 small sinkholes (diameter and depth less than 100 m)； (2) In lithology, Guizhou karst Tiankeng is mainly composed of early Triassic Yongning town formation, Yelang formation, lower Triassic Luolou formation plus Ziyun formation and middle Triassic Xiaomitang formation plus Liangshuijing formation, including Triassic thick massive limestone, middle Carboniferous and lower Permian thick massive limestone； (3)The genesis of karst Tiankeng in Guizhou includes two types， collapse type and erosion type, and the former is primary； (4) This karst Tiankeng is mainly distributed in central, southern, western and northwestern Guizhou showing a trend of gradual decrease in number and scale from south to north and from west to east, and super or super-large Tiankeng concentrates in the south.

     

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