天然气地球科学

• 天然气地质学 • 上一篇    下一篇

塔里木盆地哈拉哈塘地区奥陶系顺层岩溶带高产稳产主控因素

代冬冬,孙勤华,王宏斌,郑多明,余建平,姚清洲,杨丽莎,房启飞   

  1. (1.中国石油勘探开发研究院西北分院,甘肃 兰州 730020;
    2.中国石油塔里木油田勘探开发研究院,新疆 库尔勒 841000)
  • 收稿日期:2015-05-27 修回日期:2015-07-07 出版日期:2015-09-20 发布日期:2015-09-20
  • 作者简介:代冬冬(1984-),男,湖北荆州人,工程师,硕士,主要从事石油地质综合研究. E-mail:daidongdong@petrochina.com.cn.
  • 基金资助:

    中国石油天然气股份有限公司塔里木油田分公司科研项目(编号:041014090012);国家科技重大专项(编号:2011ZX05004-004)联合资助.

Analysis Controlling Factors of High and Stable Yield of OrdovicianBedding Karst Zone in Halahatang Area,Tarim Basin

DAI Dong-dong,SUN Qin-hua,WANG Hong-bin,ZHENG Duo-ming,YU Jian-ping,YAO Qing-zhou,YANG Li-sha,FANG Qi-fei   

  1. (1.Northwest Research Institute of Petroleum Exploration&Development,PetroChina,Lanzhou 730020,China;
    2.Research Institute of Petroleum Exploration and Development,Tarim Oilfield Company,PetroChina,Korla 841000,China)
  • Received:2015-05-27 Revised:2015-07-07 Online:2015-09-20 Published:2015-09-20

摘要:

塔里木盆地哈拉哈塘地区目前已成为塔里木盆地石油增储上产的重点勘探区,而顺层岩溶带为哈拉哈塘油田的重要产量区块。顺层岩溶带奥陶系一间房组碳酸盐岩油气产量的75%靠22%的高产稳产井支撑,然而哈拉哈塘地区储层非均质性强,单井产能、产量变化快,给油气高产稳产带来很大困难。通过对研究区断裂、明暗河、微地貌、储集体规模与高产稳产关系的分析,明确了顺层岩溶带风化壳储层主要受到断裂和明河的影响。断裂不仅控制了储层发育,也控制了裂缝发育,同时也是油气运聚的有利通道,是顺层岩溶带奥陶系碳酸盐岩高产稳产的主控因素之一。暗河系统、正地貌单元、储集体规模大是顺层岩溶带奥陶系碳酸盐岩高产稳产的其他主控因素。

关键词: 断裂, 明河, 暗河系统, 正地貌, 储集体规模, 哈拉哈塘地区

Abstract:

Halahatang area has become the focus oil exploration area in Tarim Basin.Efficient well accounts for only 22% of total wells in bedding karst belt,but accounted for 74% of total production,so analysis controlling factors of high and stable yield of Ordovician bedding karst zone has an important guiding significance for the exploration of Halahatang area.Bedding karst weathering crust reservoir is mainly affected by the faults and rivers.Faults not only control the development of reservoir,but also control the crack development,which is the migration and accumulation of oil and gas’ favorable channels,that is one of the main controlling factors of Ordovician carbonate rock with high and stable yield.Underground river system,positive landform unit,reservoir scale is also the main controlling factors of Ordovician carbonate karst area along the layer of high and stable yield.

Key words: Fracture, River, Underground river system, Positive landform, Reservoir scale, Halahatang area

中图分类号: 

  • TE122.1

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