首页> 外文期刊>Journal of Asian earth sciences >Origin and accumulation mechanisms of petroleum in the Carboniferous volcanic rocks of the Kebai Fault zone, Western Junggar Basin, China
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Origin and accumulation mechanisms of petroleum in the Carboniferous volcanic rocks of the Kebai Fault zone, Western Junggar Basin, China

机译:准Jung尔盆地西部克白断裂带石炭系火山岩中石油成因与成藏机理

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The Kebai Fault zone of the West Junggar Basin in northwestern China is a unique region to gain insights on the formation of large-scale petroleum reservoirs in volcanic rocks of the western Central Asian Orogenic Belt. Carboniferous volcanic rocks are widespread in the Kebai Fault zone and consist of basalt, basaltic andesite, andesite, tuff, volcanic breccia, sandy conglomerate and metamorphic rocks. The volcanic oil reservoirs are characterized by multiple sources and multi-stage charge and filling history, characteristic of a complex petroleum. system. Geochemical analysis of the reservoir oil, hydrocarbon inclusions and source rocks associated with these volcanic rocks was conducted to better constrain the oil source, the petroleum filling history, and the dominant mechanisms controlling the petroleum accumulation. Reservoir oil geochemistry indicates that the oil contained in the Carboniferous volcanic rocks of the Kebai Fault zone is a mixture. The oil is primarily derived from the source rock of the Permian Fengcheng Formation (P(1)f), and secondarily from the Permian Lower Wuerhe Formation (P(2)w). Compared with the P(2)w source rock, P(1)f exhibits lower values of C-19 IT/C-23 TT, C19+20TT/Sigma TT, Ts/(Ts + Tm) and alpha alpha alpha-20R sterane C-27/C-28 ratios but higher values of TT C-23/C-21, HHI, gammacerane/alpha beta C-30 hopane, hopane (20S) C-34/C-33, C-29 beta beta/(beta beta + alpha alpha), and C-29 20S/(20S + 20R) ratios. Three major stages of oil charge occurred in the Carboniferous, in the Middle Triassic, Late Triassic to Early Jurassic, and in the Middle Jurassic to Late Jurassic periods, respectively. Most of the oil charged during the first stage was lost, while moderately and highly mature oils were generated and accumulated during the second and third stages. Oil migration and accumulation in the large-scale stratigraphic reservoir was primarily controlled by the top Carboniferous unconformity with better porosity and high oil enrichment developed near the unconformity. Secondary dissolution pores and fractures are the two major reservoir storage-space types in the reservoirs. Structural highs and reservoirs near the unconformity are two favorable oil accumulation places. The recognition of the large-scale Carboniferous volcanic reservoirs in the Kebai Fault zone and understanding of the associated petroleum accumulation mechanisms provide new insights for exploring various types of volcanic reservoir plays in old volcanic provinces, and will undoubtedly encourage future oil and gas exploration of deeper strata in the region and basins elsewhere with similar settings. (C) 2016 Elsevier Ltd. All rights reserved.
机译:中国西北部西准gar尔盆地的克白断裂带是一个独特的地区,可深入了解中亚西部造山带西部火山岩中的大型石油储层。石炭系火山岩分布在克白断裂带,由玄武岩,玄武质安山岩,安山岩,凝灰岩,火山角砾岩,砂砾岩和变质岩组成。火山油储层的特征是多源,多阶段充注和充注历史,这是复杂石油的特征。系统。对储集油,与这些火山岩有关的烃类包裹体和烃源岩进行了地球化学分析,以更好地约束油源,石油充注历史以及控制油气成藏的主要机制。储层石油地球化学表明,克白断裂带石炭纪火山岩中所含的石油是一种混合物。该油主要来自二叠系凤城组(P(1)f)的烃源岩,其次来自二叠系下乌尔河组(P(2)w)。与P(2)w烃源岩相比,P(1)f的C-19 IT / C-23 TT,C19 + 20TT / Sigma TT,Ts /(Ts + Tm)和alpha alpha alpha-20R值更低甾烷C-27 / C-28的比率,但TT C-23 / C-21,HHI,γ-甘油/αβC-30 ane烷,hop烷(20S)C-34 / C-33,C-29 betaβ的值较高/(beta beta + alpha alpha)和C-29 20S /(20S + 20R)比率。在石炭纪,中三叠纪,三叠纪晚期至侏罗纪早期以及中侏罗纪至侏罗纪晚期分别发生了三个主要的充油阶段。在第一阶段注入的大部分油都流失了,而在第二阶段和第三阶段则生成并积累了中度和高度成熟的油。大型地层油藏中的运移和聚集主要受顶部石炭系不整合面控制,孔隙度较高,并且在不整合面附近发育了高含油量。次生溶蚀孔隙和裂缝是储层中两种主要的储集空间类型。不整合面附近的构造高压和储层是两个有利的成藏地点。对克白断裂带大型石炭纪火山岩油藏的认识和对相关油气成藏机制的了解,为探索古老火山省的各种类型的火山岩油藏发挥了新的见解,无疑将鼓励未来对更深层的油气勘探该地区的地层和其他地区的盆地具有相似的环境。 (C)2016 Elsevier Ltd.保留所有权利。

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