＂Continuous＂ tight gas reservoirs are those reservoirs which develop in widespread tight sandstones with a continuous distribution of natural gas. In this paper, we summarize the geological features of the source ro...＂Continuous＂ tight gas reservoirs are those reservoirs which develop in widespread tight sandstones with a continuous distribution of natural gas. In this paper, we summarize the geological features of the source rocks and ＂＇continuous＂ tight gas reservoirs in the Xujiahe Formation of the middle- south transition region, Sichuan Basin. The source rocks of the Xul Member and reservoir rocks of the Xu2 Member are thick （Xul Member： 40 m, Xu2 Member： 120 m） and are distributed continuously in this study area. The results of drilled wells show that the widespread sandstone reservoirs of the Xu2 Member are charged with natural gas. Therefore, the natural gas reservoirs of the Xu2 Member in the middle-south transition region are ＂continuous＂ tight gas reservoirs. The accumulation of ＂continuous＂ tight gas reservoirs is controlled by an adequate driving force of the pressure differences between source rocks and reservoirs, which is demonstrated by a ＂one-dimensional＂ physical simulation experiment. In this simulation, the natural gas of＂continuous＂ tight gas reservoirs moves tbrward with no preferential petroleum migration pathways （PPMP）, and the natural gas saturation of＂continuous＂ tight gas reservoirs is higher than that of conventional reservoirs.展开更多
主要根据南充气温和降水资料,利用相关分析、差积曲线法和交叉列联表χ2分析,研究了川中丘陵区近50年气候变化及与ENSO的关系。结果表明,川中丘陵区的气温和降水与ENSO有关,La Ni a年份年降水增加,非ENSO状态的夏季气温偏高;年降水和夏...主要根据南充气温和降水资料,利用相关分析、差积曲线法和交叉列联表χ2分析,研究了川中丘陵区近50年气候变化及与ENSO的关系。结果表明,川中丘陵区的气温和降水与ENSO有关,La Ni a年份年降水增加,非ENSO状态的夏季气温偏高;年降水和夏季降水极不稳定,夏季和秋季降水变化有一定的反相关系,从80年代初到90年代中期经历了较强的偏冷阶段。展开更多
基金supported by the National Major Grant of"Accumulation Law,Key Technologies and Evaluations of the Stratigraphic Reservoirs"(No.2008ZX05000-001) from the Research Institute of Petroleum Exploration & Development,PetroChina
文摘＂Continuous＂ tight gas reservoirs are those reservoirs which develop in widespread tight sandstones with a continuous distribution of natural gas. In this paper, we summarize the geological features of the source rocks and ＂＇continuous＂ tight gas reservoirs in the Xujiahe Formation of the middle- south transition region, Sichuan Basin. The source rocks of the Xul Member and reservoir rocks of the Xu2 Member are thick （Xul Member： 40 m, Xu2 Member： 120 m） and are distributed continuously in this study area. The results of drilled wells show that the widespread sandstone reservoirs of the Xu2 Member are charged with natural gas. Therefore, the natural gas reservoirs of the Xu2 Member in the middle-south transition region are ＂continuous＂ tight gas reservoirs. The accumulation of ＂continuous＂ tight gas reservoirs is controlled by an adequate driving force of the pressure differences between source rocks and reservoirs, which is demonstrated by a ＂one-dimensional＂ physical simulation experiment. In this simulation, the natural gas of＂continuous＂ tight gas reservoirs moves tbrward with no preferential petroleum migration pathways （PPMP）, and the natural gas saturation of＂continuous＂ tight gas reservoirs is higher than that of conventional reservoirs.
文摘主要根据南充气温和降水资料,利用相关分析、差积曲线法和交叉列联表χ2分析,研究了川中丘陵区近50年气候变化及与ENSO的关系。结果表明,川中丘陵区的气温和降水与ENSO有关,La Ni a年份年降水增加,非ENSO状态的夏季气温偏高;年降水和夏季降水极不稳定,夏季和秋季降水变化有一定的反相关系,从80年代初到90年代中期经历了较强的偏冷阶段。
