论因民组的若干沉积建造特征  

Some Characteristics of Sedimentation of the Yinmin Formation

作　　者：华仁民[1] 

机构地区：[1]南京大学地球科学系

出　　处：《沉积学报》1993年第1期32-40,共9页Acta Sedimentologica Sinica

摘　　要：本文从因民组的裂谷构造背景出发,论述了其中长石砂岩的发育等沉积建造特证,认为因民组是我国境内最老的大陆红层之一;对因民组内各种角砾岩进行了初步分类,并着重讨论了袭谷条件下同生角砾岩的特征及成因;提出因民组应属陆相磨拉石建造而不是海相复理石建造。The Yinmin Formation is a unit of the Middle Proterozoic Kunyang Group distributed in Yunnan and Sichuan provinces, and is considered to be the as source bed of the wellknown Dongchuan type copper deposits. It is lithologically composed of breccia and or conglomerate, sandstone, siltstone, slate, and some dolomite at the upper part. The well-developed arkose and the distinctive purple colour reveals that the Yinmin Formation is a continental red bed which was formed in rift environment, and was the lowest unit of a transgressive series of rift sedimentation. Different kinds of breccia (and conglomerate) are developed in the Yinmin Formation which is. a special feature reflecting the rift background and later structural deformation. The present paper gives a preliminary classification of these breccia and describes some of them, with an emphasis on the process of formation of the syngenetic breccia. It is concluded that the Yinmin Formation as a whole is of terrestrial facies but not a marine facies nor a flysch.

关 键 词：因民组 大陆红星 长石砂岩 沉积 

分 类 号：P512.2[天文地球—地质学]