低勘探海域中建南盆地烃源岩早期预测

    Early prediction of source rocks in Zhongjiannan Basin in low exploration area

    • 摘要: 烃源岩是油气生成的物质基础。利用最新采集的高品质二维地震资料和综合研究成果,在中建南盆地内划分出4套地震层序,识别了5个不整合地震反射界面。通过分析盆地沉积演化特征,推测中建南盆地发育3套烃源岩,分别为中始新统湖相烃源岩、上始新统—渐新统湖相和海陆交互相烃源岩以及下—中中新统海相烃源岩。通过对其周边盆地进行类比分析,厘定了3套烃源岩的地震相特征;对不同沉积相带泥岩百分含量进行赋值,最终判识推测了中建南盆地新生代3套烃源岩泥岩厚度及分布特征。本研究可为盆地下一步油气资源评价、有利二级构造带分析和勘探部署提供参考。

       

      Abstract: Source rocks are the material basis for oil and gas generation. Based on newly acquired high-quality two-dimensional seismic data and comprehensive research results, we recognized four sets of seismic sequences and five stratigraphic units controlled by unconformity in seismic reflection interface in the Zhongjiannan Basin, and analyzed the sedimentary evolution characteristics of the basin. It is speculated that three sets of main source rocks were developed in the Zhongjiannan Basin, i.e. Middle Eocene lacustrine source rocks, Upper Eocene-Oligocene lacustrine source rocks and ocean-land facies source rocks, and Lower Miocene to Upper Miocene marine source rocks. Through analogical analysis of the surrounding basins, the seismic facies characteristics of the three sets of source rocks were determined. The thickness and distribution of mudstone in the three sets were estimated in the percentage of mud in different sedimentary facies zones. This study provided a reference for evaluating oil and gas resources, analyzing favorable secondary structural zones, and exploration planning.

       

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