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机构地区:[1]中国地质大学地球科学与资源学院,北京100083 [2]中国科学院地质与地球物理研究所,北京100101
出 处:《现代地质》2009年第3期385-393,共9页Geoscience
基 金:国家自然科学基金项目(40674046)
摘 要:黄海构造是地质领域重要的研究课题,尤其是南黄海油气勘探工作虽然经过了30多年的研究与勘探,但至今仍进展不大;因此,如何突破该区油气勘探的难题引起普遍关注。黄海地区在新生代经历过2次近南北向的缩短与挤压(135~52Ma,23~0.78Ma)和2次近东西向的缩短与挤压(52—23Ma,0.78Ma-)。新生代的4个构造期对于油气资源的形成、运移和保存产生了重大的影响。白垩纪-古新世是形成盆-山体系的雏型时期,始新世-渐新世(52~23Ma)是生油层形成的主要时期,中新世一早更新世(23~0.78Ma)的构造作用使NNE向的先存断裂成为油气运移的良好通道,中更新世以来(0.78Ma-)近东西向的挤压使NNE向的断层闭合,为油气的保存创造了良好的条件。建议大力加强南黄海地区NNE向的先存断裂与古近系相交部位及其上部的油气勘探工作。To study the tectonics of the Yellow Sea is the common concern project. Although the oil-gas exploration has undergone more than 30 years in South Yellow Sea, the exploration progress of that is not successful. There are two nearly N-S trending shortening and compression epochs (135 -52 Ma and 23 -0. 78 Ma) and two nearly E-W trending shortening and compression stages (52 -23 Ma and 0. 78 Ma - ) at the Yellow Sea and its adjacent areas during Cenozoic. Four tectonic epochs during Cenozoic have important influences on forming, migrating and preserving oil-gas reservoirs. An embryonic form of the basin-range framework occured in Cretaceous and Paleocene (135 -52 Ma), and Eocene-Oligocene (52 -23 Ma) is the main forming epoch for oil-gas source. During Miocene-Early Pleistocene (23 -0. 78 Ma), tectonism caused favorable passage for oil-gas migration along NNE trending faults. Since Middle Pleistocene (0. 78 Ma - ) the NNE trending faults are closed and make a good condition for reservation of oil-gas, controlled by E-W trending shortening. The authors suggest to pay more attentions to the oil-gas exploration at the intersections between NNE trending existing faults and Eocene-Oligocene systems, and also pay attentions to the upper parts in South Yellow Sea area.
分 类 号:P542[天文地球—构造地质学] TE121.1[天文地球—地质学]
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