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ANALYSIS OF CENOZOIC TECTONICS IN THE BOHAI BAY BASIN PROVINCE

机译:渤海湾盆地省新生代构造分析

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Bohai Bay basin province is a major Cenozoic rift basin, which includs 3 geographical units, namely, northern North China Plain, sea area of Bohai Bay and Xialiaohe Plain. The data of petroleum exploration have clearly indicated that the architecture of the basin can be divided into 3 tectonic levels. The lower level, the basement of basin which consists of pre-Eogene formation, is dissected by a great number of basement faults (mostly normal faults), and have constructed a series of half-grabens (or grabens) and half-horsts (or horsts). The middle level, which consists of Eogene filling up in the half-grabens and grabens, is involved in the deformation of basement structure and result in many cover faults, the upper level, which consists of Neogene and Quaternary, is not involved in the deformation of basement structure, and overlies as a blanket upon the whole basin province including both grabens and horsts so that the whole Bohai Bay basin province forms a united major depression.
机译:渤海湾盆地省是一个主要的新生代裂谷流域,包括3个地理单位,即北华北平原,渤海湾海域和西亚霍伊平原。 石油勘探数据已经清楚地表明,盆地的结构可以分为3个构造水平。 较低的水平,由主要地层组成的盆地的基础,由大量的地下室故障(大多数正常断层)解剖,并且已经构建了一系列半妊娠(或GRABENS)和半horsts(或 霍斯特斯)。 中间水平包括在半身粘贴和妊娠中填充的eogene填充,涉及地下室结构的变形,并导致许多封面故障,由Neogene和第四纪组成的上层不涉及变形 地下室结构,并作为整个盆地省的毯子,包括Grabens和Horsts,使整个渤海湾盆地省形成联合国家萧条。

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