贵州紫云猴场早二叠世茅口晚期生物礁主体部位的地质剖面新资料  

New Geological Section Data of the Main Parts of Bioherms in Late Maokou Age of Early Permian in Houchang of Ziyun County, Guizhou

作　　者：陈文一[1] 

机构地区：[1]贵州省地矿局地质科学研究所

出　　处：《贵州地质》1991年第4期335-341,共7页Guizhou Geology

摘　　要：本文是对紫云猴场早二叠世晚期生物礁主体部位逐一分层,发现在28m内具有14种生物,可按岩性组合、生物组合划分三个对称旋回,它们均属高水位沉积体系域的产物。Through an individual division of the beds of the main parts of the late bioherms of Early Permian in Houchang of Ziyun County,the author of this paper discovered that there are 14 biota in the depths of 28 meters, which can be divided into 3 symmetry cycles according to lithologic associations and bioassociations. They all belong to the products of high water gauge sedimentary system.

关 键 词：生物礁 早二叠世 地质 贵州 礁岩 

分 类 号：P588.248[天文地球—岩石学]