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Sequence Stratigraphic Characteristics of Fluvial Facies in the Guantao Formation of South Gentle Slope Belt, Huanghekou Sag

机译:武涛面部南柔软坡带武涛相的序列地层特征,黄河口凹陷

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Through the comprehensive analysis of the data related to cores, logging and seismic, the author holded that there were two kinds of sedimentary systems in the study area, which were braided river deposits and meandering river deposits. According to the sequence stratigraphy method of fluvial facies proposed by Catuneanu et al, we established sequence stratigraphic framework in the Guantao formation of south gentle slope belt, Huanghekou Sag. It was divided into 2 third-order sequences, named as SQGU and SQGL, each of the third-order sequences contains a high accommodation systems tract (HAST) and a low accommodation systems tract (LAST). On this basis, the author summarized the sedimentary sequence evolution characteristics in the Guantao formation of south gentle slope belt, Huanghekou Sag. In the period of LAST in the SQGL, there were mainly composed of braided river facies in the study area, main developed multistage compound sand body. In the period of HAST in the SQGL, there were mainly composed of meandering river facies in the study area, main developed isolated point bar sand body and a high proportion of flood plain mud. The evolution characteristic of the SQGU was similar to the SQGL. Because of the accommodation space of the SQGU was at a high level, the grain size of sandstone and the percentage of sandstone are smaller than SQGL. It is generally accepted that it was mainly composed of braided river facies in Guantao formation of Huanghekou Sag, difficult to form oil and gas reservoir due to lack of mudstone cap rock. The exploration of Guantao formation has not attracted enough attention. Through this analysis, the author thinked that two sets of meandering river deposition can provide partial sealing and created conditions for oil-gas accumulation in the Guantao formation of south gentle slope belt, Huanghekou Sag. Under the guidance of this research, we have obtaineda certain oil and gas discovery in the study area.
机译:通过对与核心,伐木和地震有关的数据的综合分析,作者认为研究区有两种沉积体系,这是编织河矿床和蜿蜒的河流沉积物。根据Catuneanu等人提出的河流相的序列地层方法,我们在南柔和坡带的瓜涛形成序列地层框架,黄河口凹陷。它被分为2个三阶序列,命名为SQGU和SQGL,每个三阶序列都包含一个高级的容纳系统散乱(Hast)和低容纳系统的道路(最后)。在此基础上,作者总结了围围南柔软坡带形成的沉积序列演化特征,黄河口凹陷。在持续的SQGL期间,主要开发了多级复合砂体的研究区中的编织河相形。在SQGL的Hast期间,主要由研究区的蜿蜒河流组成,主要发达的孤立点酒吧砂体和洪水平原泥浆的高比例。 SQGU的演变特性类似于SQGL。由于Sqgu的住宿空间处于高水平,砂岩的晶粒尺寸和砂岩的百分比小于SQGL。人们普遍认为,它主要由围王河口凹陷的编织河相形组成,由于缺乏泥岩帽岩,难以形成石油和燃气藏。卦形成的探索并没有引起足够的重视。通过这种分析,笔者认为两套蜿蜒的河流沉积可以为南方柔和坡带的瓜涛形成中的油气积累提供部分密封和创造条件,黄河口凹陷。在本研究的指导下,我们已经找到了研究区域的某些石油和天然气发现。

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