摘要
冀东、辽西是“燕山运动”的发祥地,两区同处于燕辽沉降带中,在地质上是可类比的,但在中生代火山岩凹陷区的形态、构造、地层等诸方面都存差异。差异的分界是凌源—杨杖子断裂。这些差异对矿产资源的寻找和地质单元的划分都有影响。
Yidong and Liaoxi are analogical in geology because the place of origin of 'Yanshan movement'and
they are in settling band of Yanliao, Mesozoic Era Hollow. But there are different in shape, structure and geo-
sphere of area of mesozoic era extrusive rock hollow. The boundary line of different is break between Lingyuan
and Yangzhangzi. These different have effect on finding mineral resource and dividing geology unit.
出处
《有色矿冶》
2004年第2期1-3,共3页
Non-Ferrous Mining and Metallurgy
关键词
冀东中生代火山岩凹陷
辽西中生代火山岩凹陷
地质差异
内蒙地轴
承德地块
Yidong Mesozoic Era hollow
Liaoxi Mesozoic Era hollow
geology different
Inner Mongolia axis of the earth
Chengde land block