李强, 温珍河. 南黄海盆地成因机制及其构造意义[J]. 海洋地质前沿, 2014, 30(10): 14-17.
    引用本文: 李强, 温珍河. 南黄海盆地成因机制及其构造意义[J]. 海洋地质前沿, 2014, 30(10): 14-17.
    LI Qiang, WEN Zhenhe. ORIGIN OF THE SOUTH YELLOW SEA BASIN AND ITS TECTONIC IMPLICATION[J]. Marine Geology Frontiers, 2014, 30(10): 14-17.
    Citation: LI Qiang, WEN Zhenhe. ORIGIN OF THE SOUTH YELLOW SEA BASIN AND ITS TECTONIC IMPLICATION[J]. Marine Geology Frontiers, 2014, 30(10): 14-17.

    南黄海盆地成因机制及其构造意义

    ORIGIN OF THE SOUTH YELLOW SEA BASIN AND ITS TECTONIC IMPLICATION

    • 摘要: 南黄海盆地在大地构造位置上位于下扬子准地台的东部,是我国东部重要的中新生代陆相含油气盆地。关于南黄海盆地的成因机制,现在还存在较大的争论,故对南黄海盆地的成因机制进行了讨论和总结。南黄海盆地处在特提斯构造域、亚洲构造域和滨太平洋构造域的中心位置,其形成过程中受到多种因素的影响,不同时期起到主要作用的因素不同。

       

      Abstract: The South Yellow Sea Basin, tectonically situated on the east of the Lower Yangtze Para-platform, is an important Meso-Cenozoic continental petroliferous basin in East China. There have always existed disputes about the formation mechanism of the South Yellow Sea Basin, In this paper, the origin and genetic mechanism of the South Yellow Sea Basin are discussed.The South Yellow Sea Basin is in the central location of Asian、circle Pacific and Tethys structural domains, the forming process has been influenced by many factors, different factors play a major role in different phases.

       

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