辽宁太子河流域晚元古宙青白口系震积岩的发现及其意义
REGIONAL GEOLOGY OF CHINA（1999）
Abstract
介绍了辽宁太子河流域新发现的晚元古宙青白口系南芬组震积岩的层序.该层序为原地系统震积岩,由液化泥晶脉、震褶岩、震塌岩及地裂缝等组成.这是目前在我国所发现的最低层位碳酸盐岩振动液化地震事件记录.
MoreAI Read Science
Must-Reading Tree
Example
Generate MRT to find the research sequence of this paper
Chat Paper
Summary is being generated by the instructions you defined