摘要
坳陷堆积的下辽河平原发育过程,就是地壳在地球内部产生的“反重力的”力和重力作用下,裂谷发生和具有明显阶段性演变,并不断接受堆积的物质过程。
The development of the depresion accumulating lower Liaohe River plain has been part of a mass moving process in which, under the force of gravity and that of 'antigravity' from the earth interior, rift valleys have been created in the earth crast, which bear obvious signs of graduating changes and which have been constants receiving depression
出处
《东北师大学报（自然科学版）》
CAS
CSCD
1989年第4期101-108,共8页
Journal of Northeast Normal University(Natural Science Edition)
