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塔里木盆地阿克库勒地区下奥陶统古岩溶及油气分布
引用本文:陈强路,王恕一,钱一雄,马红强.塔里木盆地阿克库勒地区下奥陶统古岩溶及油气分布[J].沉积学报,2002,20(4):633-637.
作者姓名:陈强路  王恕一  钱一雄  马红强
作者单位:1 中国地质大学资源学院,武汉,430074;
基金项目:国家科技攻关项目,99-111-02-02,
摘    要:下奥陶统碳酸盐岩是阿克库勒地区主要含油气层,岩溶作用是影响奥陶系储层发育的最主要因素。本文详细论述了该区下奥陶统发育多期岩溶,海西早期是主岩溶期,该期岩溶主要形成于表生大气淡水条件下,岩溶作用深度和范围受志留-泥盆系和上奥陶统隔水层限制。指出岩溶斜坡区的地表岩溶带及潜流岩溶带上部是有利的储层发育和油气主要富集区带。

关 键 词:塔里木盆地    阿克库勒凸起    下奥陶统    古岩溶
文章编号:1000-0550(2002)04-0633-06
收稿时间:2001-05-14
修稿时间:2001年5月14日

Paleo-karst and Distribution of Oil and Gas of Lower Ordovician in Akekule Area , Tarim Basin
CHEN Qiang lu , WANG Shu yi QIAN Yi xiong MA Hong qiang.Paleo-karst and Distribution of Oil and Gas of Lower Ordovician in Akekule Area , Tarim Basin[J].Acta Sedimentologica Sinica,2002,20(4):633-637.
Authors:CHEN Qiang lu  WANG Shu yi QIAN Yi xiong MA Hong qiang
Institution:1 The Faculty of Earth Resources,China University of Geosciences,Wuhan 430074;2 Wuxi Research Institute of Experimental Geology, SINOPEC, Wuxi Jiangsu 214151
Abstract:Lower Ordovician carbonate rock is the major reservoir in Akekule area of Tarim Basin, and karst is the most important factor influencing Ordovician reservoir. The authors point out that karst in the study area is paleo supergene karst mainly controlled by fresh water karst and with multi stage features. The development depth is restricted by waterproof stratum of Silurian Devonian and Upper Ordovician rocks. We also suppose out that the surface of karst zone and upper phreatic karst zone in karst slope unit is favorable reservoir and enrichment region of oil and gas.
Keywords:Tarim basin    Akekule uplift    Lower Ordovician    paleo  karst
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