摘要
通过对福建省三叠纪地层基本特征的野外观察及室内分析，认为中三叠世的安仁组属于与印支造山运动同造山期的磨拉石建造；而晚三叠世的大坑村组、文宾山组、焦坑组则是代表新构造旋回底部层序沉积的磨拉石建造。
Based on the field observation of the basic characteristics of Triassic strata and in-dooranalysis in Fujian Province, the authors suggested that the Middle Triassic Anren Formationbelongs to the molasse formation of Indosinian synorogenic period, and the Dakengcun,Wenbinshan and Jiaokeng Formations belong to the molasse formations of sequence bottomof the later tectonic cyele.
出处
《福建地质》
1998年第1期12-15,共4页
Geology of Fujian
