首页 | 本学科首页   官方微博 | 高级检索  
     检索      

塔里木盆地库鲁克塔格地区下寒武统西大山组深水沉积序列
引用本文:姜雪,程日辉,王璞珺,刘万洙.塔里木盆地库鲁克塔格地区下寒武统西大山组深水沉积序列[J].地质科技情报,2010,29(2).
作者姓名:姜雪  程日辉  王璞珺  刘万洙
作者单位:1. 中国石油大学油气资源与探测国家重点实验室,北京,102249;吉林大学地球科学学院,长春,130061
2. 吉林大学地球科学学院,长春,130061
基金项目:中国石油化工股份有限公司西部新区勘探指挥部项目"塔里木盆地孔雀河地区沉积体系有效烃源岩与选区评价研究" 
摘    要:以野外剖面为基础,结合区域地质资料,对塔里木盆地库鲁克塔格地区下寒武统西大山组的深水沉积进行了分析,确定了其沉积环境和海平面变化情况。研究表明,库鲁克塔格北部西大山组发育的层状硅质岩及石膏的成因与火山活动及断裂活动具有密切关系,瘤状灰岩是在经洋流及海水溶解作用后经压实作用而形成的;西大山组是一个向上变浅的沉积序列,沉积环境由次深海过渡为台前斜坡;西大山组所反映的长周期海平面变化背景为海侵末期至海退初期。

关 键 词:塔里木盆地  库鲁克塔格  西大山组  深水沉积序列

Deep-Water Sedimentary Sequence of Xidashan Formation, Early Cambrian in Kuruktag , Tarim Basin
JIANG Xue,CHENG Ri-hui,WANG Pu-jun,LIU Wan-zhu.Deep-Water Sedimentary Sequence of Xidashan Formation, Early Cambrian in Kuruktag , Tarim Basin[J].Geological Science and Technology Information,2010,29(2).
Authors:JIANG Xue  CHENG Ri-hui  WANG Pu-jun  LIU Wan-zhu
Abstract:On the basis of field outcrops and regional geological data, the paper analysed the deep-water deposits of Xidashan Formation of Early Cambrian in Kuruktag, Tarim Basin, in order to realize the sedimentary environment and sea level changes. It suggests that:(1) The genesis of the bedded siliceous rocks and gypsum of Xidashan Formation in north of Kuruktag should be related to volcanic activities and tectonic activities, while the nodular limestone is formed by compaction after being dissolved by current and sea water.(2) Xidashan Formation is a upward shallowing sedimentary sequence, whose sedimentary environment changed from bathyal environment to fore-platform slope. (3) Long-cycle sea-level changes background reflected by Xidashan Formation is from final stage of marine transgression to early stage of marine regression.
Keywords:Tarim Basin  Kuruktag  Xidashan Formation  deep-water sedimentary sequence
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号