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和田河气田奥陶系碳酸盐岩气藏类型再认识及其意义
引用本文:邬光辉,朱海燕,张立平,王春和,周波,高力. 和田河气田奥陶系碳酸盐岩气藏类型再认识及其意义[J]. 天然气工业, 2011, 31(7): 5-10. DOI: 10.3787/j.issn.1000-0976.2011.07.002
作者姓名:邬光辉  朱海燕  张立平  王春和  周波  高力
作者单位:1.中国石油勘探开发研究院;2.中国石油塔里木油田公司
基金项目:国家科技专项“四川、塔里木等盆地及邻区海相碳酸盐岩大油气田形成条件、关键技术及目标评价”(编号:2008ZX05004-04)
摘    要:和田河气田是在塔里木盆地发现和探明的第一个古生界碳酸盐岩大气田,但围绕其周缘钻探的一系列局部构造相继失利,迫切需要对其气藏类型重新进行认识。为此,通过分析该区地层水、天然气及储层特征,发现大多出水井段为非地层水或少量局部封存水,无大面积的块状底水;天然气性质在纵、横向上有变化,具有明显不均一性;古潜山储层不受现今构造高程控制,非均质性强,横向变化大,连通性差,以相对孤立的缝洞体储层为主。气藏模式分析结果表明:该区奥陶系气藏为沿古潜山顶面分布、受缝洞体储层控制的非构造型气藏,是和田河气田周缘奥陶系勘探的主攻类型,南部的麦盖提斜坡区发育奥陶系风化壳岩溶储层,是寻找大面积非构造油气藏的有利方向。

关 键 词:塔里木盆地  奥陶纪  碳酸盐岩  非构造油气藏  储层特征  地层水分析  风化壳岩溶  勘探方向

Recognition of the Ordovician carbonate reservoir types of the Hetianhe Gas Field,Tarim Basin,and Its Significance
Wu Guanghui,Zhu Haiyan,Zhang Liping,Wang Chunhe,Zhou Bo,Gao Li. Recognition of the Ordovician carbonate reservoir types of the Hetianhe Gas Field,Tarim Basin,and Its Significance[J]. Natural Gas Industry, 2011, 31(7): 5-10. DOI: 10.3787/j.issn.1000-0976.2011.07.002
Authors:Wu Guanghui  Zhu Haiyan  Zhang Liping  Wang Chunhe  Zhou Bo  Gao Li
Affiliation:1.Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China; 2.Research Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Kuerle, Xinjiang 841000, China
Abstract:The Paleozoic carbonate reservoirs are first discovered in the Hetianhe of the Tarim Basin,but the successive failures in the exploratory drilling at its marginal areas compel us to get a new understanding of reservoir types there.Therefore,through a deep investigation into formation water,characteristics of natural gas and reservoirs,and types of gas reservoirs,the following conclusions are presented herein in this paper.(1) Non-formation water or a small amount of local connate water presents at most wate...
Keywords:Tarim Basin  Ordovician  carbonate  pool  reservoir  exploration  
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