攀西地区“沧浪铺组”乌龙箐段与红井哨段接触关系再认识

RECONSIDERATION ON THE CONTACT BETWEEN THE WULONGQING MEMBER AND THE HONGJINGSHAO MEMBER OF “THE CANGLANGPU FORMATION” IN PANXI REGION

应用综合地层学的理论和方法，详细研究了攀西地区“沧浪铺组”乌龙箐段与红井哨段的地层接触关系，指出两段之间应为假整合接触。这对攀西地区，乃至整个寒武纪盆地的地质发展史和地层学研究具有重要意义。

Applying the theory and method of comprehensive stratigraphy,this paper has discussed the disconformable contact between the Wulongqing Member and the Hongjingshao Member of“the Canglangpu Formation” in detail This disconformable contact is of significance to the understanding of geologic history and stratigraphy of Panxi region