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准噶尔盆地玛湖凹陷下二叠统风城组烃源岩热演化及沉积古环境评价
引用本文:蒋中发,江梦雅,陈海龙,刘龙松,王学勇,卞保力,李娜.准噶尔盆地玛湖凹陷下二叠统风城组烃源岩热演化及沉积古环境评价[J].现代地质,2022,36(4):1118-1130.
作者姓名:蒋中发  江梦雅  陈海龙  刘龙松  王学勇  卞保力  李娜
作者单位:中国石油新疆油田分公司勘探开发研究院,新疆 克拉玛依 834000
基金项目:中国石油天然气集团公司重大科技专项“准噶尔盆地凹陷区下组合轻质油与天然气成藏规律”(2021DJ0206)
摘    要:近期准噶尔盆地玛湖凹陷南斜坡地区多口探井钻遇风城组厚层烃源岩,为重新认识玛湖凹陷风城组烃源岩带来了契机,搜集玛湖凹陷南部、北部5口重点探井资料,经分析取得了以下认识:(1)风城组烃源岩在玛湖凹陷内广泛发育,综合玛北、玛南地球化学参数表明其为一套Ⅱ型优质烃源岩;(2)综合现今地温、热解、生物标志物、族组分等参数,认为玛湖凹陷及其周缘地区4 350 m以深的风城组烃源岩处于成熟阶段,4 800 m以深处于高成熟演化阶段,玛湖凹陷风城组烃源岩大范围处于生油高峰期;(3)综合多个生物标志物参数,玛北地区风城组烃源岩为咸化还原沉积,玛南地区风城组二段烃源岩为咸化半还原沉积,风三段烃源岩为半咸化-半还原沉积,陆源有机质输入较多。研究区风城组沉积古环境总体表现出早中期咸化、晚期淡化,北部咸化还原程度高于南部的规律。研究结果对玛湖凹陷风城组后续致密油、页岩油勘探部署提供了理论依据。

关 键 词:玛湖凹陷  风城组  成熟度  古环境  
收稿时间:2021-07-15
修稿时间:2021-12-07

Thermal and Paleoenvironment Evolution of the Fengcheng Formation of Permian in Mahu Depression,Junggar Basin
JIANG Zhongfa,JIANG Mengya,CHEN Hailong,LIU Longsong,WANG Xueyong,BIAN Baoli,LI Na.Thermal and Paleoenvironment Evolution of the Fengcheng Formation of Permian in Mahu Depression,Junggar Basin[J].Geoscience——Journal of Graduate School,China University of Geosciences,2022,36(4):1118-1130.
Authors:JIANG Zhongfa  JIANG Mengya  CHEN Hailong  LIU Longsong  WANG Xueyong  BIAN Baoli  LI Na
Institution:Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000,China
Abstract:Several exploration wells were recently drilled into the thick hydrocarbon source rock of Fengcheng Formation in the southern slope of Mahu Depression in the Junggar Basin, which brings an opportunity to reveal the source rocks there. This study collected data from five key exploration wells in the southern and northern Mahu Depression, and obtained the following findings: (1) the Fengcheng Formation source rocks are widely distributed in Mahu Depression, and the northern and southern Mahu Depression geochemical parameters show that the source rocks are of II-type and high-quality; (2) based on current geothermal, pyrolysis, biomarkers and group compositions, the Fengcheng Formation source rocks around the Mahu Depression entered mature and highly-mature stage at below 4,350 m and 4,800 m, respectively, and have entered the oil generation peak widely; (3) integrating multiple biomarker parameters, the Fengcheng Formation source rocks in northern Mahu Depression were deposited in a saline and reducing environment, and the source rocks of the Fengcheng Formation (2nd member) in southern Mahu Depression were deposited in a saline and semi-reducing environment, whilst the 3rd member (also in southern Mahu Depression) were deposited in a brackish and semi-reducing environment, and adsorbed more terrigenous organic matter. Paleoenvironment of the local Fengcheng Formation is featured by salinization (early) and desalinization (end), and the degree of salinity and reduction in the north is higher than that in the south. This study provides a theoretical basis for the subsequent exploration and deployment of tight oil and shale oil for the Fengcheng Formation in Mahu Depression.
Keywords:Mahu Depression  Fengcheng Formation  thermal maturity  paleoenvironment  
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