摘要
本文对雪峰古陆下古生界缺失带是否存在、加里东期构造变形特征、深部地球物理资料以及早古生代岩相带变窄作了研究，确定了该区确实存在加里东期推覆构造，并对其基本特征进行了研究。
This paper studies the lower palaeozoic group lacked belt which exists or not,the characteristics of structural deformationin in Caledonian stage,the data of deep geophysical field and the narrowed early palaeozoic lithofacies belt. It is confirmed that the Caledonian nappe structure exist in Xuefeng paleoland,and the characteristics of nappe structure is studied.
出处
《华东地质学院学报》
1996年第3期201-210,共10页
Journal of East China Geological Institute
基金
国家自然科学基金
