Research on Limestone 'dragon scale felsenmeer' and its causes in Wansheng District of Chongqing

摘要

This paper makes a research on "dragon scale felsenmeer" in Wansheng District in Chongqing by analyzing geological structure of limestone area in which "Crackle" has formed in South China through referring large amounts of data, and combing with the analysis of Ordovician sedimentary environment and diagenetic conditions. Based on the analysis, this study has made an initial judgment that "dragon scale felsenmeer" is controlled by sedimentary pattern in regional structure dynamic and sedimentary environment, and the pressure in diagenetic conditions.