东营凹陷低电阻率油层地质主控因素分析

2007年 14卷 第05期
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Primary geologic origins analysis on low resistivity
zone in Dongying Depression
蔡秋龙
Cai Qiulong
胜利油田分公司地质科学研究院,山东东营257015
Geological Scientific Research Institute,
Shengli Oilfield Company, SINOPEC, Dongying 257015,
China
针对高矿化度地层水型低电阻率油层,运用岩电实验分析资料和典型区块地质
特征解剖相结合的方法,定量评价地层水对储层视电阻率的影响及地质主控因素分析。研究表
明,地层水矿化度高达50 g/L时可形成该类低电阻率油层,沉积水环境和构造断裂是该类低
电阻率油层的地质主控因素,沙四段、沙三中下储层和大的构造断裂附近为东营凹陷有利的低
电阻率油层发育区带。
In view of the low resistivity zones of high formation water
salinity, the influences of formation water on reservoir apparent
resisitivity were quantitatively evaluated and the primary
geology origins were analyzed through petrophysical
experimental analysis and anatomy of representative blocks爷
geologic features. The results show that the low resistivity
zones of high formation water salinity can be come into being
when the formation water salinity is greater than 50gramme per
litre, that the sedimentary water environment and structure
fracture are primary geology origins of low resistivity zones of
high formation water salinity,which mostly distribute in the
reservoir of the fourth section of Shahejie Formation, base of
the middle part of the third section in Shahejie Formation and
the vicinity of large structure fractures in Dongying
Depression.
东营凹陷; 低电阻率油层; 沉积水环境; 构造断裂;
Dongying Depression, low resistivity zone,
sedimentary water environment, structure fracture.;