范昌育教授

教授 博士生导师 硕士生导师

出生日期:1982-07-29

电子邮箱:

入职时间:2012-07-01

所在单位:地质学系

学历:博士研究生毕业

办公地点:

性别:男

联系方式:微信:fancy33041371

学位:博士学位

在职信息:在职

主要任职:

其他任职:

毕业院校:西北大学

所属院系:

学科: 矿产普查与勘探

当前位置: 中文主页 >> 论文成果

Flow pathway and evolution of water and oil along reverse faults in the northwestern Sichuan Basin, China

点击次数:

影响因子:0.0

DOI码:10.1036/10261816501

所属单位:西北大学

教研室:石油教研室

发表刊物:AAPG Bulletin

刊物所在地:美国

摘要:As a three-dimensional geological body, a fault zone has a complex internal structure. Disputes remain over flow pathways of fluids within fault zones. Well and seismic data cannot be used to effectively identify the internal structures of a fault zone. Furthermore, continuous core sampling in fault zones is commonly limited. Fewer studies of flow pathways along reverse faults are done in a sedimentary basin. Through extensive outcrop observations, sampling, and measurements in the northwestern Sichuan Basin of China, this study enhances our understanding of fluid evolution and the main pathway of vertical fluid flow along a reverse fault. In the studied carbonates, deep hot brine initially entered the fault zone and migrated upward along the fault core, then moved to shallow strata, mixed with meteoric water, and cooled in the fault zone. In the studied sandstone and shale, a paleo-oil pool formed in the fault damage zone. After that, forced by uplift and reactivation, oil migrated into the fault core along fractures and was cooled, washed, biodegraded, and oxidized by meteoric water. In the sandstone–sandstone juxtaposition faults, the oil shows are distinctly different between hanging wall and footwall. Fault rocks (sand and shale gouges) that developed along the principal slip surface seem to have prevented fluid flow across the fault. This evidence suggests that fault core and inner damaged zone are the main pathways of vertical fluid flow along the investigated reverse fault zone.

论文类型:期刊论文

学科门类:工学

一级学科:地质资源与地质工程

卷号:103

期号:5

页面范围:1153–1177

是否译文:

发表时间:2019-05-01

收录刊物:SCI

第一作者:范昌育

上一条: Originand distribution of irregular oil-water contacts in tight sandstones, Chang 8(1) Member, Longdong area, Ordos Basin, China

下一条: 柴达木盆地北缘鄂博梁构造带超压形成机制与高压气、水层成因