论全吉运动

On the Quanji movement

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。
- 全吉运动 /
- 角度不整合
Abstract: 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.
- movement of Quanji /
- angular unconformity

青海地质研究所.青海省地质图说明书(1/100万)[M].1981.

成都地质学院教研室编.大地构造基础及中国区域构造概要[M].北京:地质出版社,1984.