松辽盆地外围西部上二叠统林西组岩相古地理特征
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摘要
松辽盆地外围西部上二叠统林西组主要分布于西拉木伦河断裂以北、贺根山—黑河断裂以南,以及稍北的内蒙古地区。根据野外勘察、实测剖面和岩心观察资料,建立研究区上二叠统林西组沉积亚相岩性组合模式,明确晚二叠世林西组岩相古地理特征。结果表明:研究区上二叠统林西组主要发育湖泊、扇三角洲、河流3种沉积相,以及滨浅湖、半深湖、扇三角洲平原、扇三角洲前缘、辫状河、滨浅海6种沉积亚相,以滨浅湖亚相为主,滨浅海亚相分布局限,在林西县官地剖面顶部出现。松辽盆地西部上二叠统林西组,构成以西拉木伦河与贺根山—黑河断裂为主要控制区的、以南北向物源供给为主的滨浅湖—扇三角洲—河流沉积体系。该结果对松辽盆地外围西部晚古生代油气勘探具有重要意义。
In the western periphery of Songliao Basin,the Linxi Formation is mainly distributed on the north of the Xilamulun River,south of the Hegen Mountain-Hei River Faults and in the Inner Mongolia Region on the north.In this paper,authors set up a lithology combination model of Permian series Linxi Formation sedimentary subfacies in research area,and defined the lithofacies palaeogeography characteristics of Upper Permian through a lot of field geological explorations and section measurements.The results indicate that there are three types of sedimentary facies in the Upper Permian Linxi Formation:lake facies,fan delta facies and river facies.There are also 6 kinds of sedimentary subfacies,including semi-deep lake subfacies,fan delta plain subfacies,fan delta front subfacies,braided river subfacies littoral shallow sea subfacies and littoral shallow lake subfacies mainly.The offshore subfacies coastal and shallow marine facies distribut limited,only at the top of the profile in Linxi county magistrate.In the western periphery of Songliao Basin,the distribution of Linxi Formation is mainly controlled by the Xilamulun River and Hegen Mountain-Hei River Faults.The main sources of supplyment are from south and north.It forms a shallow lake-fan delta-river sedimentary system.This result is of great significance for Late Paleozoic oil and gas exploration in the western periphery of Songliao Basin.
In the western periphery of Songliao Basin,the Linxi Formation is mainly distributed on the north of the Xilamulun River,south of the Hegen Mountain-Hei River Faults and in the Inner Mongolia Region on the north.In this paper,authors set up a lithology combination model of Permian series Linxi Formation sedimentary subfacies in research area,and defined the lithofacies palaeogeography characteristics of Upper Permian through a lot of field geological explorations and section measurements.The results indicate that there are three types of sedimentary facies in the Upper Permian Linxi Formation:lake facies,fan delta facies and river facies.There are also 6 kinds of sedimentary subfacies,including semi-deep lake subfacies,fan delta plain subfacies,fan delta front subfacies,braided river subfacies littoral shallow sea subfacies and littoral shallow lake subfacies mainly.The offshore subfacies coastal and shallow marine facies distribut limited,only at the top of the profile in Linxi county magistrate.In the western periphery of Songliao Basin,the distribution of Linxi Formation is mainly controlled by the Xilamulun River and Hegen Mountain-Hei River Faults.The main sources of supplyment are from south and north.It forms a shallow lake-fan delta-river sedimentary system.This result is of great significance for Late Paleozoic oil and gas exploration in the western periphery of Songliao Basin.
引文
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[4]曲希玉,张满利,刘立,等.中国东北地区晚二叠世岩相古地理特征[J].古地理学报,2013,15(5):679-692.QU Xiyu,ZHANG Manli,LIU Li,et al.Lithofacies palaeogeography characteristics of the Late Permian in Northeast China[J].Journal of Palaeogeography,2013,15(5):679-692.
[5]李晓海,郑月娟,宗文明,等.内蒙古阿鲁科尔沁旗陶海营子地区林西组沉积环境[J].地质与资源,2014,23(4):357-363.LI Xiaohai,ZHENG Yuejuan,ZONG Wenming,et al.The sedimentary environment of Linxi Formation in Taohaiyingzi Area of Aruhorqin Qi,Inner Mongolia[J].Geology and Resources,2014,23(4):357-363.
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[8]翟大兴,张永生,田树刚,等.兴蒙地区晚二叠世林西组灰岩微量元素与碳、氧同位素特征及沉积环境讨论[J].地球学报,2015,36(3):333-343.ZHAI Daxing,ZHANG Yongsheng,TIAN Shugang,et al.The Late Permian sedimentary environments of Linxi Formation in Xingmeng Area:constraints from carbon and oxygen isotopes and trace elements[J].Acta Geoscientica Sinica,2015,36(3):333-343.
[9]翟大兴,张永生,田树刚,等.内蒙古林西地区上二叠统林西组沉积环境与演变[J].古地理学报,2015,17(3):359-370.ZHAI Daxing,ZHANG Yongsheng,TIAN Shugang,et al.Sedimentary environment and evolution of the Upper Permian Linxi Formation in Linxi Area Inner Mongolia[J].Journal of Palaeogeography,2015,17(3):359-370.
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[12]朱占平,张明杨,孙雷,等.内蒙古索伦-林西地区林西组泥页岩储层特征[J].石油实验地质,2015,37(3):354-360.ZHU Zhanping,ZHANG Mingyang,SUN Lei,et al.Reservoir characteristics of mud shales from Upper Permian Linxi Formation in Suolun-Linxi Area,Inner Mongolia[J].Petroleum Geology Experiment,2015,37(3):354-360.
[13]苏飞,李臻,张健,等.内蒙古突泉盆地突D2井上二叠统林西组烃源岩新发现[J].地质与资源,2017,26(3):268-274.SU Fei,LI Zhen,ZHANG Jian,et al.Discovery of the soure rock from Upper Permain Linxi Formation in Tuquan Basin,Inner Mongolia[J].Geology and Resources,2017,26(3):268-274.
[14]徐民.内蒙古东部霍林郭勒-西乌旗地区林西组砂岩物源分析及构造意义[D].长春:吉林大学,2017:1-63.XU Min.The provenance analysis and tectonic significance of sandstones in Linxi Formation in Huolinguole-Xi Ujimqin Area,Eastern Inner Mongolia[D].Changchun:Jilin University,2017:1-63.
[15]张渝金,张超,郭威,等.内蒙古阿鲁科尔沁旗林西组植物化石新材料[J].地质论评,2017,63(增刊1):291-292.ZHANG Yujin,ZHANG Chao,GUO Wei,et al.New material of Late Permian plants from Linxi Formation of Arukeqinqi,Inner Mongolia,China[J].Geological Review,2017,63(Supp.1):291-292.
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