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| 1 | Reservoir characteristics,formation mechanisms and petroleum exploration potential of volcanic rocks in China显示文摘Characterized by complex lithology and strong heterogeneity, volcanic reservoirs in China developed three reservoir space types: primary pores, secondary pores and fractures. The formation of reservoir space went through the cooling and solidification stage(including blast fragmentation, crystallization differentiation and solidification)and the epidiagenesis stage(including metasomatism, filling, weathering and leaching, formation fluid dissolution and tectonism). Primary pores were formed at the solidification stage, which laid the foundation for the development and transformation of effective reservoirs. Secondary pores were formed at the epidiagenesis stage, with key factors as weathering and leaching, formation fluid dissolution and tectonism. In China, Mesozoic–Cenozoicvolcanic rocks developed in the Songliao Basin and Bohai Bay Basin in the east and Late Paleozoic volcanic rocks developed in the Junggar Basin, Santanghu Basin and Tarim Basin in the west. There are primary volcanic reservoirs and secondary volcanic reservoirs in these volcanic rocks, which have good accumulation conditions and great exploration potential. | Zhi-Guo Mao Ru-Kai Zhu Jing-Lan Luo Jing-Hong Wang Zhan-Hai Du Ling Su Shao-Min Zhang | 2015 | Petroleum Science2015，12，1： | 12 |
| 2 | 东营凹陷营26断层调节带特征及其对油气分布的控制作用显示文摘为揭示复杂断块油田小型断层调节带的特征并明确其对油气分布的控制作用,笔者利用高精度三维地震资料结合油田地质资料分析了营26块内断层的几何学、运动学和动力学特征,认为其为近东西向展布的对向叠覆—同向叠覆复合型断层调节带。西侧主断层(营1断层)与调节断层在剖面上呈多级反'Y'字形组合样式,东侧主断层(营8断层、营31断层)与调节断层为包心菜状组合;营1断层活动性减弱时,将位移量传递给营8断层、营31断层和调节断层,使区域位移有规律变化;通过力学分析认为营26北部断层调节带是在左旋张扭构造应力场作用下形成的,营26南部断层调节带是在右旋张扭构造应力场作用下形成的。结合营26块油气分布、油气来源及断裂活动性与封闭性研究,阐明了主断层沟通烃源灶和储集层,成为油源断层;调节断层停止活动时间早,封闭性好形成断块圈闭,是遮挡断层;建立了营26断层调节带油气成藏模式,预测营13井、营24井和营26井附近为有利滚动勘探开发区。 | 田飞 金强 曾翔 王端平 杨勇 | 2013 | 中国地质2013，40，4： | 6 |
| 3 | Principles of Trap Development and Characteristics of Hydrocarbon Accumulation in a Simple Slope Area of a Lacustrine Basin Margin:An Example from the Northern Section of the Western Slope of the Songliao Basin,China显示文摘The western slope of the Songliao Basin is a gently dipping monoclinal slope featured by stratum overlap, gradual change of stratum inclination and limited fault development, which formed during basin depression interrupted by a tectonic inversion stage. Structure, sedimentation and reservoir characteristics show that the development of the slope and its sand bodies' depositional genesis determined the types, distribution and evolution of traps. Up-dip wedge-out traps in distributary channels, lenticular traps in distal sand bars and sand sheets in the delta front are the main lithologic trap types and usually have thin reservoir beds, small areas, and are distributed in clusters and belts. The episode of tectonic inversion led to the formation of structural traps and combination traps. The combination traps are characterized by large numbers of thin oil-bearing beds occurring along fold belts. Matching axial directions of distributary channel sand bodies in delta fronts with channel morphology during the period between deposition of sand bodies and sealing by an unconformity above is the key to the search for large scale traps in a simple slope area. | Hongyu Wang Tailiang Fan Xuesong Fan | 2016 | Journal of Earth Science2016，27，6： | 2 |
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