摘要
针对准噶尔盆地乌夏地区地质流体分布的复杂特征,从水文地质条件和地层水化学特征分析入手,剖析了地层水与油气保存条件的关系。研究认为,处于交替阻滞带和交替停止带的二叠系、三叠系的大气水下渗阶段时间较短暂,而压榨水阶段时间较长,且受深部热液影响大,地层水以CaCl2和NaHCO3水型为主,矿化度高,钠氯系数和脱硫酸系数低,属于未破坏或微破坏型,保存条件优越,有利于油气聚集成藏。
Based on the complicated distribution of geological fluid in Wuxia area of the Junggar Basin,from the aspects of hydrogeological conditions and formation water chemical characteristics,it has been discussed in this paper the relationship between formation water and hydrocarbon preservation.Studies have suggested that,Permian and Triassic experienced short stages of atmospheric water seepage and long stages of water compression since they were in alternative blocking and stopping belts.Severely influenced by deep thermal fluids,the formation water was mainly CaCl2 and NaHCO3 types with high salinity as well as low sodium chloride and de-sulfate coefficients.It was not or seldom damaged and provided excellent conditions for the preservation of hydrocarbon.
出处
《石油实验地质》
CAS
CSCD
北大核心
2012年第1期36-39,共4页
Petroleum Geology & Experiment
基金
中国石油天然气股份有限公司重大预探项目"准噶尔盆地重点区带目标优选与评价"(070108-3)部分研究成果
关键词
矿化度
水文地质
地层水
油气保存
准噶尔盆地
salinity
hydrogeological condition
formation water
hydrocarbon preservation
Junggar Basin