2) 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。
4) large petroleum accumulation zone
大型油气聚集带
1.
Central uplift belt in Tarim basin is a typical large petroleum accumulation zone characterized by multiple sets of source rocks,various types of reservoir rocks,many kinds of traps and oil/gas pools,multistage hydrocarbon charging,and various plays.
塔里木盆地中央隆起带以发育多套烃源层系、多种储集类型、多类圈闭与油气藏、多期油气充注、多种成藏组合为基本特征,是典型的大型油气聚集带。
5) multiple oil and gas accumulation zone
复式油气聚集带
1.
Methods The relationships between pool-forming dynamic systems and multiple oil and gas accumulation zones are discussed on the basis of analysis of pool-forming dynamic systems in the eastern Zhanhua Sag.
方法 以油气成藏动力学系统的基本研究思路,探讨成藏动力学系统与复式油气聚集带的关系。
2.
The northern slope of the Yihezhuang Arch is a typical multiple oil and gas accumulation zone consisted of multiple oilbearing series and multiple reservoirs types.
义和庄凸起北坡是一个典型的多含油层系、多油藏类型的复式油气聚集带。
6) composite hydrocarbon-bearing unit
复合油气聚集带
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