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机构地区:[1]石油工业出版社,北京100011
出 处:《新疆石油地质》2004年第5期550-553,共4页Xinjiang Petroleum Geology
摘 要:中国型含油气域包括中国大陆及相邻地带,被亚洲型含油气域包裹。由于陆核面积小、活动性强,经大陆增生作用,于古生代末才形成统一的地台;中、新生代又受特提斯洋消减和关闭影响而发生裂解,使得大地构造复杂程度冠于全球。含油气域内古生代、中生代和新生代的含油气层系,在一个盆地中以叠合为特点。含油气盆地除活动大陆边缘盆地外,其余内克拉通盆地已经消失,前陆盆地和裂谷盆地也都与世界典型的盆地有区别,可称为中国式的。China-type petroleum domains include onshore China and adjacent belts,which is enwrapped by Asia-type petroleum domain. Such small, intensively active continental nucleus did not generate a unified platform by continental overgrowth until the end of the Paleozoic, and was separated by the subducted and closed Tethys Sea during Mesozoic and Neozoic period, resulting in the most complex tectonic features in the world. Within the petroleum domains, the hydrocarbon-bearing Paleozoic, Mesozoic and Neozoic sequences were superimposed in a basin. With an exception of the active continental margin basins, the intra-cratonic basins had disappeared, and the foreland basins and rift basins were different from others in the world, so they can be called China-type basins.
关 键 词:含油气域 盆地类型 塔里木盆地 渤海湾盆地 莺琼盆地
分 类 号:TE11[石油与天然气工程—油气勘探]
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