塔里木盆地大坂塔格奥陶系地层层序及沉积演化ORDOVICIAN SEQUENCE STRATIGRAPHY AND SEDIMENTOLOGY IN THE DABANTAGE AREA,TARIM BASIN
郭峰,赖生华,郭岭
摘要(Abstract):
塔里木盆地大坂塔格—一间房奥陶系剖面自下而上可划分为蓬莱坝组、鹰山组、一间房组、吐木休克组和良里塔格组,下与寒武系下丘里塔格组整合接触,顶部出露不全,为第四系覆盖。该剖面由下至上可以识别出6个三级层序,每个层序由海侵体系域和高水位体系域构成,缺少低水位体系域,密集段由深灰色—灰色泥质灰岩、泥晶灰岩等组成。碳酸盐台地为本区典型沉积,海平面升降变化是控制该区沉积相发育和分布的主要因素。
关键词(KeyWords): 层序地层;沉积演化;奥陶系;大板塔格;塔里木盆地;新疆
基金项目(Foundation): 中国石油塔里木油田分公司“塔里木油田野外地质考察基地建设(柯坪—巴楚)”项目的部分研究成果
作者(Author): 郭峰,赖生华,郭岭
DOI: 10.19839/j.cnki.dcxzz.2010.02.003
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