塔北隆起侏罗系阳霞组沉积特征THE JURASSIC FLUVIAL FACIES IN THE NORTH TARIM UPLIFT,XINJIANG
张丽娟,钟大康,李越,程明,魏燕萍
摘要(Abstract)：
塔北隆起侏罗系阳霞组下粗上细的沉积特征显示其为典型的河流相沉积,东部普惠1井序列发育最全,向轮南隆起方向具有明显的顶剥底超特征。河流沉积体系中,颗粒普遍偏粗,物源主要来自东河塘以北、英买力以西及跃南地区,英买力西部、东河塘北部以北以及跃南1、2井以南发育近源小型冲积扇,由西向东发育辫状河沉积体系。根据沉积相的空间展布模式,可预测低位域三角洲及湖泊相发育于草湖及其以东地区;阳霞组砂体分别向北部的轮台凸起、南部的中央隆起尖灭,是寻找岩性地层圈闭的有利地区。
关键词(KeyWords)： 辫状河;冲积扇;阳霞组;侏罗系;塔北隆起;新疆
基金项目(Foundation): 国家自然科学基金项目(No.40572069);; IGCP506项目支持
作者(Author): 张丽娟,钟大康,李越,程明,魏燕萍
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