中国琼东南盆地宝岛相陵水地层和三亚地层海底扇的沉积模式和源汇过程

Xingzong Yao , Congjun Feng , Hongjun Qu , Jia Chen , Mengsi Sun
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摘要

深水区是油气勘探的前沿领域之一,了解深水储层的分布和成因对成藏研究至关重要。尽管琼东南盆地宝岛斜坡已被证实富含油气生成,但在超深水区尚未发现重要油气田,深水储层的分布规律仍不清楚。以宝岛斜坡南坡区为例,采用地震反射结构分析、地震面几何学、地震属性分析、源-汇理论等地震预测方法,研究了海底扇的分布特征。研究结果表明:扇三角洲呈平行斜进反射,坍塌潜水扇呈透镜状反射,三亚地层潜水扇呈近平行片状反射。沉积物的成因可追溯到西南部的松南低隆起剥蚀区和南部隆起区。沉积物主要通过南北两个主要的切入河道系统运移,最终流入宝岛山南坡地区。地震沉积学预测方法和源汇理论的应用,为宝岛尾闾深水区油气勘探和成藏条件分析奠定了坚实的地质基础。
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Depositional pattern and source-to-sink process of submarine fans in Lingshui and Sanya formations, Baodao Sag, Qiongdongnan Basin, China

The deepwater area is one of the frontiers of oil and gas exploration, with the understanding of distribution and genesis of deepwater reservoirs being crucial for reservoir formation research. Despite Baodao Sag in the Qiongdongnan Basin being proven to be rich in hydrocarbon generation, significant oil and gas fields have yet to be discovered in the ultra-deepwater areas, and the distribution patterns of reservoirs in deep water remain unclear. Taking the southern slope area of the Baodao Sag as an example, the distribution characteristics of submarine fans are studied by employing seismic prediction methods, including seismic reflection structure analysis, seismic facies geometry, seismic attribute analysis, and the source-to-sink theory. The results show distinct characteristics: the fan delta exhibits parallel oblique progradational reflection, the slumping submarine fan displays lenticular reflection, and the submarine fan of the Sanya Formation demonstrates subparallel sheet reflection. The provenance of sediment is traced back to the denudation area of the Songnan low uplift and the Southern Uplift area in the southwest. The sediments were primarily transported through two main incised channel systems in the north and south, ultimately flowing into the southern slope area of the Baodao Sag. The application of seismic sedimentological prediction methods and source-sink theory has laid a solid geological foundation for oil and gas exploration and the analysis of reservoir forming conditions in the deepwater area of the Baodao Sag.

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