摘要
论述了对泌阳凹陷中心核桃园组向苏打湖演化过程中碳酸盐岩形成的特征、沉积相条件、沉积模式,以及碳酸盐岩的生油母质、油原岩、资源量、储集空间、油藏等。指出了老区滚动勘探开发的新领域及潜力层。
This paper expounds the characterization of forming carbonate rock during evolution from Hetaoyuan Fm in the central area of Biyang sag to Sodo Lake, conditions of sedimentary facies, sedimentation model as well as mother material of oil source in carbonate rock, oil source rock, resource quantities, reservoirs, reservoir space ets, and points out new area and potential reservoirs of the progressive exploration and development in the oil fields.
出处
《河南石油》
1996年第2期1-6,20,共7页
Henan Petroleum
基金
国家自然科学基金(编号49070105)