摘要
在阐述区域地质构造和含水系统划分的基础上,论证了川西坳陷上三叠统含水系统隶属于沉积水压系统类型,提出了研究深层水渗流场的原则和方法,并根据计算勾画了研究层水头等值线图和水动力分带图,揭示了深层水的流动特点和规律性.
Based on regional tectonics and water_bearing systems, the upper Triassic water_bearing system in Chuanxi depression may be classified as a sedimentary hydraulic system. The research method and principle for vadose field of confined deep water are also discussed, and the waterhead contour and hydrodynamic zoning maps are outlined for the study interval, by which flow regimes and rules of deep water are revealed in the depression.
出处
《中国海上油气（地质）》
2002年第5期317-321,共5页
China Offshore Oil and Gas(Geology)
基金
国家自然科学基金
关键词
水压系统类型
渗流场
上三叠统
川西坳陷
油气地质
hydraulic pressure system type
vadose field
upper Triassic
Chuanxi depression
