摘要
全吉运动发生于柴北缘地区的全吉山一带,除角度不整合的自然现象外,接触面上下岩层之岩性载然不同、变质程度迥异,同位素测试值显示,是一次强烈的区域动力变质构造运动。
The movement of Quanji was taken place at Quanji Mountain on the north margin of Qaidam basin.Besides the natural phenomenon of the discontinuity of stratum angles,the characters between the touched surfaces of upper and lower terrains are various.According to the isotope dating data,it was a strong regional dynamo-metamorphic structural movement.
出处
《西北地质》
CAS
CSCD
2003年第4期30-34,共5页
Northwestern Geology
基金
大柴旦幅
达布逊幅1/20万区调报告及<青海地质志>
关键词
全吉运动
角度不整合
movement of Quanji
angular unconformity
