准噶尔盆地吉木萨尔凹陷井井子沟组微裂缝微观特征及成因
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本文为新疆维吾尔自治区自然科学基金资助项目(编号:2021D01F39)和克拉玛依市创新环境建设计划 (创新人才)项目(编号:20232023hjcxrc0049)的成果


Microscopic characteristics and causes of micro- fractures in the Jinjinzigou Formation in Jimsar Sag, Junggar Basin
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    摘要:

    笔者等利用岩芯、薄片、扫描电镜和分析化验等资料,开展了吉木萨尔凹陷井井子沟组致密砂岩储层微裂缝特征分析,并揭示了微裂缝成因。研究表明:①基于裂缝与颗粒之间的分布关系,将井井子沟组致密砂岩储层微裂缝分为粒内缝、粒缘缝和穿粒缝3种类型,其中粒内缝最发育,穿粒缝次之,粒缘缝最不发育;利用延伸长度、面密度和开度等参数评价了3种类型微裂缝分布,研究区开启性裂缝占60%以上,以穿粒缝开启性最好。②微裂缝发育控制的因素主要有构造作用、岩石成分和结构等,微裂缝主要发育在中砂岩、细砂岩中,颗粒粒度越粗、分选越好,微裂缝越发育;储层抗压能力较弱,致使粒内缝和穿粒缝的成为主要微裂缝类型;点—线接触使得颗粒间的接触面积较小,有利于微裂缝发育。③研究区微裂缝成因主要为原生、成岩和构造成因,粒内缝为原生成因和成岩成因,粒缘缝为成岩成因和构造成因,穿粒缝为构造成因,穿粒缝有助于储层渗流能力的发育,是优质储层发育的有利因素之一。研究成果对于准噶尔盆地致密砂岩储层微裂缝的成因及优质储层评价具有指导意义,并对类似地质条件的致密储层油气勘探可以起到一定的借鉴作用。

    Abstract:

    It is generally believed that the tight sandstone reservoir has strong heterogeneity and poor physical properties, but the tight sandstone reservoir in the Jimsar Sag, Junggar Basin, has good oil and gas production. Through the core data photos, it is found that the reservoir fractures of the Jinjinzigou Formation (P2jj) in the study area are developed, most of which are filled with crude oil and calcite. Based on the microscopic thin sections and scanning electron microscope photos, it is found that most samples develop micro- fractures. Through the observation, measurement and calculation of micro- fractures under the microscope, combined with the core and regional tectonic background, the development characteristics, main controlling factors and genetic mechanism of micro- fractures were systematically analyzed, and the formation stages of micro- fractures were discussed. The research results have guiding significance for the genesis of micro- fractures in tight sandstone reservoirs and the evaluation of high- quality reservoirs in the Junggar Basin, and can be used as a reference for oil and gas exploration in tight reservoirs with similar geological conditions.Methods: In order to study the distribution characteristics and genesis of micro- fractures in tight sandstone reservoirs of the Jinjinzigou Formation (P2jj) , cast thin sections, scanning electron microscopy (SEM) and Nano Measure software were used to observe and measure the reservoirs of the Jinjinzigou Formation (P2jj) in PetroChina Xinjiang Oilfield Company. Through the observation of 226 cast thin sections and SEM images, the characteristics and causes of micro- fractures were analyzed. Through the cutting relationship, development characteristics and regional tectonic background between micro- fractures, the formation stages of micro- fractures were discussed.Results: The results show that the micro- fractures in tight sandstone reservoirs of the P2jj in the Jimsar sag can be divided into three genetic types: tectonic origin, diagenetic origin and abnormal high- pressure origin. Based on the scale of micro- fractures and the relationship between micro- fractures and particles, the micro- fractures in the study area are divided into three basic types: intra- granular fractures, grain- edge fractures and penetrating fractures. Among them, intra- granular fractures are the most developed and the most important micro- fracture type in the reservoir. The second is the most developed grain- penetrating fracture. The development scale of grain- penetrating fracture in the study area is large, cutting through particles, and most of them are effective fractures. The grain boundary seam is less developed, which is mainly developed between the particles, and the connectivity is better. According to the microscopic analysis, the reservoir micro- fractures in the study area are effective, and the open micro- fractures account for more than 60%. Most of the filled fractures are filled with organic matter and crude oil.Conclusions: Based on the analysis, the micro- fractures in the reservoir of Jinjinzigou Formation (P2jj) are mainly affected by diagenesis and tectonism, and their development degree is mainly controlled by internal factors (sandstone grain size, rock debris composition, interstitial content and contact relationship between particles and particles) and external factors (tectonism). Based on the analysis of tectonic stages, there are at least 3 stages of micro- fractures in the study area, which are primary fractures, dissolution fractures, early filling fractures re- split fractures and late cutting fractures. In general, micro- fractures are not developed in tight sandstone reservoirs in the study area. In medium- fine sandstone, micro- fractures are developed in siltstone, and micro- fractures are more developed. In argillaceous siltstone, the development of micro- fractures is weak, and in mudstone, micro- fractures are basically not developed.

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陈晓轩,李雯,徐倩茹,耿梅,王智忠,韩宝,赵晓东.2025.准噶尔盆地吉木萨尔凹陷井井子沟组微裂缝微观特征及成因[J].地质论评,71(1):181-191,[DOI].
CHEN Xiaoxuan, LI Wen, XU Qianru, GENG Mei, WANG Zhizhong, HAN Bao, ZHAO Xiaodong.2025. Microscopic characteristics and causes of micro- fractures in the Jinjinzigou Formation in Jimsar Sag, Junggar Basin[J]. Geological Review,71(1):181-191.

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  • 收稿日期:2024-04-26
  • 最后修改日期:2024-07-01
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  • 在线发布日期: 2025-01-19
  • 出版日期: 2025-01-15