1) hydrocarbon accumulation
油气聚集
1.
Paleostructure characteristics of Yanshan stage and its relationship with hydrocarbon accumulation in Chishui and neighboring area.;
赤水及邻区燕山期古构造特征与油气聚集关系
2.
Control of fault activity on hydrocarbon accumulation in central Junggar Basin;
准噶尔盆地腹部断裂活动对油气聚集的控制作用
3.
Reversal degree of reversal structures and its relation with hydrocarbon accumulation;
反转构造的反转程度及其与油气聚集的关系
2) oil and gas accumulation
油气聚集
1.
Segmentation of oil and gas accumulation in Qiulitage structural belt and its forming mechanism;
秋里塔格构造带油气聚集分段性及成因机制
2.
Its impact on oil and gas accumulation has become one of the highly considered issues in petroleum geology circles.
本文在综述反转构造研究进展的基础上 ,重点对伸展盆地反转构造概念及样式、反转构造识别及其与油气聚集的关系进行了论述 ,旨在为东部伸展含油气盆地中寻找与反转构造有关的油气藏提供科学基
3) Oil-gas accumulation
油气聚集
1.
Sequence-stratigraphic framework and oil-gas accumulation rule in Songliao Basin.;
松辽盆地层序地层格架及油气聚集规律
2.
By comprehensive analysis of regional geology and structure on the north of Chaidamu basin, the paper summarizes oil-gas accumulation pattern.
结果表明 :侏罗系生烃中心控制了油气藏的分布 ,油气聚集在北西走向的鄂博梁、冷湖—南八仙、赛南—绿南 3个构造带上 ;指出了冷湖—南八仙构造带是最有利的含油气带 ,赛南—绿南山前逆冲推覆带具有广阔的油气勘探前景 。
3.
Bozhong area has different oil-gas accumulation characteristics from the adjacent onshore oil fields.
同时，两种断裂系统、垒堑相间的构造格局、晚期油气运移的多样性造就了渤中坳陷上第三系丰富多彩的油气藏类型和大规模的油气聚集。
4) petroleum accumulation
油气聚集
1.
Reservoir controlling mechanism and petroleum accumulation model for consequent fault and antithetic fault in Fushan Depression of Hainan area;
海南福山凹陷顺向和反向断裂控藏机理及油气聚集模式
2.
Relationship between deformation structure and petroleum accumulation and preservation,Qiangtang Basin,Tibet;
羌塘盆地变形构造与油气聚集保存关系
3.
The formation and the distribution of the pivot positions of structural activities in Talimu Basin, and their control effect on petroleum accumulation are analyzed.
为了更好地指导塔里木盆地碳酸盐岩的勘探实践 ,进一步认识叠合盆地油气富集规律 ,从塔里木盆地构造活动枢纽部位的形成、分布以及对油气聚集的控制入手 ,剖析了碳酸盐岩油气藏的宏观分布规律 。
6) hydrocarbon accumulation zone
油气聚集带
1.
Diversified characteristics and anisotropism of marine carbonate reservoirs result in the fact that the controlling factors of hydrocarbon accumulation zones are different from that of the clastic rocks in the traditional nonmarine basin.
海相碳酸盐岩储层多类型及非均质性强的特点,决定了其油气聚集带与以往陆相盆地碎屑岩油气聚集带的控制因素有显著差异,碳酸盐岩的油气聚集并不是简单地受二级构造带的控制。
补充资料：油气聚集带
| 油气聚集带 oil and gas accumulation zones 同一构造带或地层岩相变化带中，油气聚集条件相似的一系列油气藏或油气田的总和。聚集带内的油气是由邻近生油层运移至此形成。油气聚集带形成过程的主要控制因素是构造因素和地层因素。常见的类型有：①背斜构造型油气聚集带。油气田带在构造上为一背斜带（群）。这是最常见的类型，而且常拥有大的油气田，如中国大庆长垣。②断裂型油气聚集带。包括断块、同生正断层逆牵引背斜油气聚集带和逆冲断层带。③盐（泥）丘型油气聚集带。包括盐丘、泥火山、泥底辟等背斜带。④潜山型油气聚集带。组成潜山的岩石类型有碳酸盐岩、碎屑岩、火山岩和结晶岩等，以碳酸盐岩潜山对油气聚集最为有利。中国任丘潜山油气聚集带即属于碳酸盐岩潜山。⑤生物礁油气聚集带。从古生代至新生代地层中都发现有礁油气聚集。⑥地层不整合油气聚集带。指不整合面以上为不渗透层遮挡，其下形成的油气聚集带。⑦超覆、岩性油气聚集带。超覆是由于水进造成的，油气的聚集就形成地层超覆油气聚集带；岩性油气聚集带指储集层的岩性或物性侧向变化形成的油气藏趋向带，包括岩性尖灭和透镜体聚集带。 |
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参考词条