摘要
鄂尔多斯盆地天环凹陷北部地区上古生界气水分布规律十分复杂,主要表现为平面上无统一的气水界面,剖面上气水多层叠置。针对这一问题,通过对该区岩心、构造裂缝观察和显微裂缝观测及构造沉积微相、输导体系、气水分布规律及主控因素的研究,配合地应力与流体势、构造裂缝预测等技术手段,明确了研究区气水分布的主要控制因素,建立了该区天然气成藏模式。研究表明:天然气常富集在地应力相对低值区、构造裂缝密度高值区、分流河道主河道及微幅构造的高部位;水体主要富存于分流河道边部、河道底部及微幅构造低部位;沉积微相类型、裂缝类型及发育程度、地应力的相对高低及微幅构造,是天环凹陷北部上古生界气水分布的主控因素。研究结果可为天环凹陷下一步天然气勘探部署提供依据。
The complicated Upper Paleozoic gas-water distribution in northern Tianhuan Depression of Ordos Basin is mainly characterized by no lateral uniform gas-water interface and overlying gas-water layers in the longitudinal direction.Based on core analysis,structural fracture and microscopic fracture observation,transmission system,gas -water distribution pattern and main-controlling factors,the predictions of geo-stress,fluid potential and structural fracture and other technical means were used to clarify the main-controlling factors for gas-water distribution and establish the corresponding gas accumnlation patterns in this urea.Research indicates that natural usually enriched in the relatively low geo-stress area,high structural fracture density area,drainage line of distributary channel and high-part of micro-structure.The aquifer mainly distributes in the side of distributary channel,the channel bottom and the low-part of micro-structure.Sedimentary microfacies,fracture type and development level,geo-stress and micro-structure are considered as the main-controlling factors for the Upper Paleozoic gas-water distribution in northern Tianhuan Depression.This research could provide certain reference for the further natural gas exploration and development in the Tianhuan Depression.
作者
王怀厂
任德生
候云东
张辉
Wang Huaichang;Ren Desheng;Hou Yundong;Zhang Hui(Petro China Changqing Oilfield Company,Xi'an,Shaanxi 710018,China;Beijing Oil Valley Technology Development Corporation,Beijing 100084,China)
出处
《特种油气藏》
CAS
CSCD
北大核心
2018年第6期32-36,共5页
Special Oil & Gas Reservoirs
基金
中国石油科技重大专项“鄂尔多斯盆地天然气富集规律、目标评价与勘探关键技术”(2016E-0502).
关键词
地应力
构造裂缝
气水分布
上古生界
天环地区
鄂尔多斯盆地
geo-stress
structural fracture
gas-water distribution
Upper Paleozoic
Tianhuan
Ordos Basin