新疆东昆仑卡尔瓦西地区二叠纪树维门科组地层序列及沉积特征  

Stratigraphic sequence and sedimentary characteristics of Permian Shuweimenke Formation in Kaerwaxi area of east Kunlun mountains of Xinjiang Province

作　　者：刘越[1] 张学海[1] 王聚胜[1] 缪树森 詹天宇 肖依琳 

机构地区：[1]吉林省地质调查院,吉林长春130061 [2]吉林省地质环境监测总站,吉林长春130021

出　　处：《吉林地质》2016年第1期12-14,44,共4页Jilin Geology

基　　金：中国地质调查局项目(1212011120532)资助

摘　　要：对新疆东昆仑卡尔瓦西地区二叠纪树维门科组地层序列及其实地测制剖面进行了描述,记录了该组地层的岩石组合与横向变化特征。研究区树维门科组主要为一套碳酸盐岩建造,局部夹碎屑岩、火山碎屑岩的沉积序列。通过分析该套地层岩石沉积特征,指出该组地层沉积环境及沉积相。Describe strata sequence and measured section exposed of Shuweimenke Formation of Permian in Kaerwaxi area of east of Kunlun mountains of Xinjiang Province. Record the rock combination and lateral variation characteristics of the group formation. Research area Shuweimenke formation mainly is a set of carbonate rocks sedimentary sequence, local contains clastic rocks and volcanic clastic rocks. According to analysis the rocks sedimentary characteristics of the strata, Points out that the strata formation sedimentary environment and sedimentary facies.

关 键 词：新疆 东昆仑 树维门科组 地层序列 沉积特征 

分 类 号：P588.14[天文地球—岩石学]