Natural gas accumulation conditions and exploration directions of Carboniferous clastic rocks in the northeastern margin of Junggar Basin, China

Yanzhao Wei , Abulimiti Yiming , Weian Wu , Aicheng Wu , Fan Yang , Chaowei Liu , Zesheng Wang , Boyu Zhou
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Abstract

The Carboniferous strata in the northeastern Junggar Basin are an important exploration field for natural gas in the basin. However, volcanic rocks have long been the primary exploration target. In contrast, the exploration and research of clastic rocks associated with source formations have been largely overlooked, resulting in an insufficient understanding of the reservoir forming conditions and exploration potential of Carboniferous clastic rocks. Through the evaluation of Carboniferous source rocks, effective source stove characterization, clastic reservoir evaluation, oil and gas source correlation, and reservoir formation model construction in this region, three key findings have been made. First, the Carboniferous in the northeastern Junggar Basin has developed three sets of high-quality gas source rocks: the Dishuiquan Formation, the Songkalsu B Member, and the Shiqiantan Formation. These formations correspond to three hydrocarbon source centers: the Sannan–Dishuiquan Sag, the Wucaiwan Sag–Dajing area, and the Dongdao Haizi Sag–Baijiahai High. Second, the Carboniferous system in the northeast has developed multiple types of large-scale reservoirs, including sand conglomerates, sandstones, turbidites, dolomitic rocks, and shale. These reservoirs are generally characterized by low porosity to ultra-low porosity and low permeability to ultra-low permeability reservoirs. There is a dissolution pore development zone at depths of 2900–4500 m. Third, a comparison of oil and gas sources reveals that all three sets of gas source rocks contribute to the natural gas found in the northeast, with obvious characteristics of near-source reservoir formation. The Carboniferous clastic rocks host two types of natural gas reservoirs: unconventional and conventional near-source reservoirs. It is predicted that there is an orderly accumulation pattern of shale gas, tight sandstone gas, and conventional natural gas reservoirs. This study reveals that the Carboniferous clastic rock source and reservoir configuration in the northeastern Junggar Basin is highly favorable, and the natural gas reservoirs in source and near-source clastic rocks represent important exploration directions.
中国准噶尔盆地东北缘石炭系碎屑岩天然气赋存条件及勘探方向
准噶尔盆地东北部的石炭纪地层是该盆地重要的天然气勘探区。但长期以来,火山岩一直是主要的勘探目标。相比之下,与源地层相关的碎屑岩的勘探和研究却在很大程度上被忽视,导致人们对石炭纪碎屑岩的储层形成条件和勘探潜力认识不足。通过对该地区石炭纪源岩的评价、有效的源炉特征描述、碎屑岩储层评价、油气源相关性研究和储层形成模型构建,取得了三项重要发现。首先,准噶尔盆地东北部石炭系发育了三套优质气源岩:滴水泉地层、松卡尔苏B层和石阡滩地层。这些地层分别对应着三个油气源中心:三南-滴水泉地层、五彩湾地层-大井地区、东道海子地层-白家海高地。其次,东北石炭系发育了多种类型的大型储层,包括砂砾岩、砂岩、浊积岩、白云质岩和页岩。这些储层一般具有低孔隙度到超低孔隙度、低渗透率到超低渗透率储层的特征。第三,通过油气源对比发现,三组气源岩都对东北部发现的天然气有贡献,具有明显的近源成藏特征。石炭纪碎屑岩蕴藏着两种类型的天然气储层:非常规储层和常规近源储层。据预测,页岩气、致密砂岩气和常规天然气储层存在有序的聚集模式。该研究揭示了准噶尔盆地东北部石炭系碎屑岩岩源和储层构造的有利条件,岩源和近源碎屑岩天然气储层是重要的勘探方向。
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