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东海陆架盆地鱼山凸起构造演化和油气远景探讨
引用本文:李国山,杨娟,高兆红,佘玉伟. 东海陆架盆地鱼山凸起构造演化和油气远景探讨[J]. 海洋石油, 2003, 23(3): 44-48
作者姓名:李国山  杨娟  高兆红  佘玉伟
作者单位:1. 上海海洋石油钻井工程公司,上海,200137
2. 中石化,上海海洋油气分公司,研究院,上海,200120
摘    要:鱼山凸起主要经历了坳陷、隆起抬升及区域披覆等三个时期的构造演化,中生代为沉积凹陷,新生代由于火山岩活动而成为凸起。鱼山凸起目前保存有厚达5000m的沉积层,这些地层为鱼山凸起提供了较好的生储盖条件。据地层、断裂、岩浆活动等资料分析,认为鱼山凸起具备了较好的生、储、盖和圈闭条件,应具有较好的油气远景。

关 键 词:东海陆架盆地  鱼山凸起  构造演化  油气远景
文章编号:1008-2336(2003)03-0044-05
修稿时间:2003-01-15

Tectonic Evolution and Hydrocarbon Potential in Yushan Uplift, the East China Sea
Abstract:The tectonic evolution can be divided into three stages in Yushan uplift. They are depression, tumescence and regional overlap. Yushan Uplift was trough in Mesozoic and uplift in Cenozoic because of the volcanicity. The sedimentary deposit has a thickness of more than 5000m in Yushan Uplift. According to the condition of source rock, reservoir, cap rock and trap, the oil and gas accumulation can be formed in Yushan Uplift.
Keywords:the East China Sea  Yushan Uplift  tectonic evolution  hydrocarbon potential
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