[1]郑小鹏,汪淑洁,郝龙,等.苏里格气田南区马五5亚段气水特征研究与判识[J].新疆石油地质,2018,(02):158.[doi:10.7657/XJPG20180205]
 ZHENG Xiaopeng,WANG Shujie,HAO Long,et al.Research and Identification of Gas and Water Characteristics in Ma-55 Submember in the Southern District of Sulige Gas Field[J].Xinjiang Petroleum Geology,2018,(02):158.[doi:10.7657/XJPG20180205]
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苏里格气田南区马五5亚段气水特征研究与判识()
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《新疆石油地质》[ISSN:1001-3873/CN:65-1107/TE]

卷:
期数:
2018年02期
页码:
158
栏目:
出版日期:
2018-04-01

文章信息/Info

Title:
Research and Identification of Gas and Water Characteristics in Ma-55 Submember in the Southern District of Sulige Gas Field
文章编号:
1001-3873(2018)02-0158-05
作者:
郑小鹏汪淑洁郝龙胡薇薇刘道天王晔
(中国石油 长庆油田分公司 a.勘探开发研究院;b.低渗透油气田勘探开发国家工程实验室,西安 710018)
Author(s):
ZHENG Xiaopeng WANG Shujie HAO Long HU Weiwei LIU Daotian WANG Ye
(PetroChina Changqing Oilfield Company, a.Research Institute of Exploration and Development; b.National Engineering Laboratory for Exploration and Development of Low Permeability Oil/Gas Fields, Xian, Shaanxi 710018, China)
关键词:
苏里格气田南区奥陶系马家沟组气水特征水体类型分布模式
Keywords:
Sulige gas field southern district Ordovician Majiagou formation gas/water characteristic water type distribution pattern
分类号:
TE124
DOI:
10.7657/XJPG20180205
文献标志码:
A
摘要:
苏里格气田南区下奥陶统马家沟组马五5亚段发育海相碳酸盐岩储集层,气藏无明显气水界面,但开发过程中气井均存在不同程度产水。通过地层水化学特征分析、测井曲线重叠法和交会图法,明确了地层水体类型、分布模式。结果表明,马五5亚段地层水属于封存较好的古代残余海水,存在底部滞留水、气水同层和透镜状水体3种分布模式,其中水层和气水层的深侧向电阻率界限为266 Ω·m,气水层和气层的深侧向电阻率界限为710 Ω·m
Abstract:
Marine carbonate reservoirs are developed in Ma-55 submember of the Lower Ordovician Majiagou formation in the southern district of Sulige gas field, which have no obvious gas-water interface. But gas wells produce water during the development process. Based on indepth analysis of chemical characteristics of formation water, logging curve overlapping and cross-plot methods, the paper determines the formation water type and distribution pattern. The results show that the formation water in Ma-55 submember belongs to well-sealed ancient residual seawater and 3 distribution patterns exist in the submember including retained water at the bottom, gas and water in the same layer and lenticular water, among which the boundary of deep lateral resistivity between aquifer and gas-water zone is 266 Ω·m and that between gas-water zone and gas zone is 710 Ω·m

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更新日期/Last Update: 2018-03-29