中国东北松辽盆地沙河子组分段特征及地质意义:对陆相含油气沉积盆地的启示

    Segmental characteristics and geological significance of the Shahezi Formation of the Songliao Basin, NE China: implications for terrestrial hydrocarbon-bearing sedimentary basins

    • 摘要: 徐家围子断陷是松辽盆地北部深层天然气资源最富集的地区,也是松辽盆地北部勘探程度最高的含气断陷。下白垩统沙河子组地层是松辽盆地徐家围子断陷的主要烃源岩,研究其地质和地球物理特征对深层资源勘探开发至关重要。位于中国东北部的松科二井钻探深度达7 018 m,获得了最完整连续的断陷层岩芯,为分析沙河子组地层提供了重要数据。本文研究根据松科二井的最新岩芯测试和测录井成果,重新统计并厘定了沙河子组地层分层层序及深部资源特征。松科二井揭示的沙河子组地层的顶、底年龄分别约为112 Ma和118 Ma,属于Aptian中期-Albian早期,是松辽盆地断陷层油气生产的重要时期。基于测井资料,厘定沙河子组地层厚度为2 624.01 m(岩芯深度3 335.99~5 960.00 m),并将沙河子组从底部到顶部划分为SQ1~SQ5五个三级层序。其中,SQ5层序烃源岩发育,成熟度高,处于高成熟-过成熟阶段,发育Ⅲ型干酪根。在SQ5层序内检测出35层气测异常,累计厚度79 m,暗色泥岩累计厚度占该层序地层厚度的59%,最具深层天然气勘探潜力,SQ2层序次之。基于上述研究,本文提出了沙河子组地层的沉积演化模式,为全球海陆相沉积对比研究提供了新视野,同时,加强对松辽盆地深部沙河子组非常规油气资源评价研究,对松辽盆地油气勘探向深部拓展具有重要的引领和示范意义。

       

      Abstract: The Xujiaweizi Fault Depression is the most abundant area of deep natural gas in the northern part of the Songliao Basin, and it is also the most explored gas-bearing fault depression in the region. The Lower Cretaceous Shahezi Formation serve as the primary hydrocarbon source rock of the Xujiaweizi Fault Depression within the Songliao Basin, making it crucial of the investigation of its geological and geophysical characteristics for the exploration and exploitation of deep-seated resources. The Well SK2, located in northeast China, is drilled to a depth of 7 018 m, yielding the most complete and continuous core of the fault depression, which provide essential data for the analysis of the Shahezi Formation’s stratigraphy. This study redefines the stratigraphic sequence and deep resource attributes of the Shahezi Formation based on the latest cores testing and logging outcomes from the Well SK2. The top and bottom ages of the Shahezi Formation revealed by the Well SK2 are about 112 Ma and 118 Ma, respectively, which belong to the middle Aptian-early Albian period, which is a significant period for hydrocarbon production in the fault layers of the Songliao Basin. Based on the logging data, the thickness of the Shahezi Formation is determined to be 2 624.01 meters (core depth 3 335.99-5 960.00 m), and the Shahezi Formation is divided into five tertiary sequences SQ1-SQ5 from the bottom to the top. SQ5 sequence has well-developed hydrocarbon source rock, with a high degree of maturity, exhibiting high maturity to over-maturity, characterized by type Ⅲ kerogen. In SQ5 sequence, 35 layers of gas measurement anomalies are detected, with a cumulative thickness of 79 m, and the cumulative thickness of dark mudstone accounted for 59% of the stratigraphic thickness of the sequence, which is the most potential for deep natural gas exploration, followed by SQ2 sequence. Based on the above study, this paper proposes a sedimentary evolution model of the Shahezi Formation, which provides a new vision for the comparative analysis of global marine and land sedimentation. Strengthening the study on evaluating unconventional oil and gas resources of the deep Shahezi Formation of the Songliao Basin is of great significance in leading and demonstrating the expansion of the Songliao Basin’s oil and gas exploration to the deep part of the Basin.

       

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