Geochemistry of formation water and its controlling factors: A case study on the Shiwu Depression of Songliao Basin, NE China | |
Xiang CF; Xie XN; Xia B | |
2003-11-09 | |
会议日期 | 2003-11-9 |
会议地点 | WUHAN, PEOPLES R CHINA |
英文摘要 | It is a common way to trace the fluid flow and hydrocarbon accumulation by studying on the geochemistry of formation water. This paper focused on the space distribution of the geochemical features of the formation water in Shiwu depression and its indication of the water-rock interaction processes. The fluid dynamic fields control the space distribution of the formation water. Due to the penetration of the meteoric water, the salinity is below 4500 mg/L at the basin margin and the severely faulted central ridge and increased basin-ward to 7000-10000 mg/L. The vertical change of the formation water can be subdivided into 3 zones, which correspond respectively to the free replacing zone (depth<1250 m), the obstructive replacing zone (1250 m |
会议录 | International Symposium on Water Resources and the Urban Environment |
语种 | 英语 |
内容类型 | 会议论文 |
源URL | [http://210.77.94.230:8080/handle/344008/9407] |
专题 | 广州地球化学研究所_中科院广州地化所(-2008) |
推荐引用方式 GB/T 7714 | Xiang CF,Xie XN,Xia B. Geochemistry of formation water and its controlling factors: A case study on the Shiwu Depression of Songliao Basin, NE China[C]. 见:. WUHAN, PEOPLES R CHINA. 2003-11-9. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论