摘要
野外考察中发现庐山羊角岭的泥砾混杂堆积体中发育有推挤构造、滑动构造以及巨大岩块的沉陷构造等,因而认为该泥砾混杂堆积体属Lawson(1981)的冰碛物分类中的次生的消融冰碛(Secondary meltout till)。
In the diamictoon of Yangjiaoling, Lushan, Jiangxi Province, the author has recognized structural features as the push (thrust and shear) structure, glide (sediment flow and gravitational slump)structure and collapse structure with huge blocks.
Therefore, the author holbs that the diamicton in Yangjiaoling, Lushan, is the secondary meltout till in the classification of the tills proposed by Lawson (1981).
出处
《地质论评》
CAS
CSCD
北大核心
1990年第2期125-129,共5页
Geological Review
