摘要
本文以现代层序地层学理论为指导 ,通过对其米级旋回层序特征和沉积相序特征的分析 ,论述了固阳地区增隆昌组风暴岩的沉积特征。同时本文对风暴岩的成因及构造意义进行了探讨。
Based on the theory of the sequence stratigraphy, the characteristics of the m-grade cycle sequence and the sequence of the sedimentary facies in the Zhenlongchang Formation, Zhaertaishan Groupe in Guyang area, the sedimentary characteristics of the tempestites in the Zhenlongchang formation were expounded. The cause and tectornic meaning of the tempestites also be discussed in the paper.
出处
《内蒙古地质》
2001年第1期8-11,共4页
Geology of Inner Mongolia
关键词
固阳
增隆昌组
风暴岩
Guyang area
Zhenlongchong Formation
Tempestites.
