鄂尔多斯盆地陇东地区二叠系山西组—石盒子组母岩类型和构造背景
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摘要
通过岩石学及地球化学分析方法,对鄂尔多斯盆地陇东地区二叠系山西组1段—石盒子组8段碎屑岩物源区的母岩类型和构造属性进行分析。研究结果表明:山1段和盒8段的砂岩碎屑组成相似,具有基本相同的物源区组成,它们在构造背景、物源及物源特征上具有很好的继承性;砂岩碎屑颗粒镜下特征及石英阴极发光颜色显示母岩主要为变质岩和火成岩;轻矿物特征反映物源与再循环造山带源区中的碰撞缝合线及褶皱—逆掩带物源区密切相关;研究区与北秦岭地区秦岭群和宽坪群斜长石种类一致;构造环境判别图解反映物源区长期受被动大陆边缘物源影响,到晚古生代后期有向主动大陆边缘转换的趋势;源岩判别图解显示物源区主要是长英质岩石;山1段、盒8段沉积岩的REE配分模式均呈右倾型且基本相互平行,与北秦岭地区秦岭群、宽坪群变质岩的稀土元素配分模式相似;锆石U-Pb同位素定年结果显示物源主要来自元古代,有少部分来自晚古生代。综合分析认为研究区主要受被动大陆边缘物源影响,其次为主动大陆边缘物源,母岩主要为北秦岭下元古界秦岭群的片麻岩、石英岩等和中、上元古界宽坪群的绿泥石片岩、阳起石片岩,其次为北秦岭造山带晚古生代岩浆岩。
Based on petrological and provenance analysis,this paper discusses tectonic property and provenance of the Member 1 of Shanxi Formation and Member 8 of Shihezi Formation of Permian in Longdong Area,Ordos Basin. The results suggest that detrital mode compositions of these two members are similar,which were formed from the same parent rocks and tectonic setting. Microscopic characteristics andCL image of quartz show that the parent rocks are metamorphic rocks and igneous rocks; Light mineral characteristics are associated with collisional suture and fold-thrust belt sources. The plagioclase An and EPMA analysis indicate that the study area and the north Qinling orogenic belt have similar plagioclase type. Tectonic discrimination plots indicate that the provenance was mainly affected by passive continental margin source until the end of Late Paleozoic,then under the influence of active continental margin. Parent rock discrimination plots suggest that the provenance was dominated by felsic rocks. The REE distribution patterns of the sedimentary rock in Shan 1 and He 8 Members are consistently declining to the right,and are very similar to those of Qinling Group and Kuanping Group in the north Qinling orogenic belt. The dating of U-Pb isotope in zircon reveal that they can be divided into two groups according to their ages,which mostly dated from Proterozoic and some from Late Paleozoic. It is concluded that the provenance mainly affected by passive continental margin,others are active continental margin sources. Furthermore,the parent rocks of Shan 1 and He 8 Members are mainly from gneiss and quartzite of Qinling Group and chlorite schist and actinolite schist of Kuanping Group in the north Qinling orogenic belt,a few from igneous rocks of late Paleozoic era in the north Qinling orogenic belt.
Based on petrological and provenance analysis,this paper discusses tectonic property and provenance of the Member 1 of Shanxi Formation and Member 8 of Shihezi Formation of Permian in Longdong Area,Ordos Basin. The results suggest that detrital mode compositions of these two members are similar,which were formed from the same parent rocks and tectonic setting. Microscopic characteristics andCL image of quartz show that the parent rocks are metamorphic rocks and igneous rocks; Light mineral characteristics are associated with collisional suture and fold-thrust belt sources. The plagioclase An and EPMA analysis indicate that the study area and the north Qinling orogenic belt have similar plagioclase type. Tectonic discrimination plots indicate that the provenance was mainly affected by passive continental margin source until the end of Late Paleozoic,then under the influence of active continental margin. Parent rock discrimination plots suggest that the provenance was dominated by felsic rocks. The REE distribution patterns of the sedimentary rock in Shan 1 and He 8 Members are consistently declining to the right,and are very similar to those of Qinling Group and Kuanping Group in the north Qinling orogenic belt. The dating of U-Pb isotope in zircon reveal that they can be divided into two groups according to their ages,which mostly dated from Proterozoic and some from Late Paleozoic. It is concluded that the provenance mainly affected by passive continental margin,others are active continental margin sources. Furthermore,the parent rocks of Shan 1 and He 8 Members are mainly from gneiss and quartzite of Qinling Group and chlorite schist and actinolite schist of Kuanping Group in the north Qinling orogenic belt,a few from igneous rocks of late Paleozoic era in the north Qinling orogenic belt.
引文
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(1)数据据长庆油田。
陈全红,李文厚,胡孝林,李克永,庞军刚,郭艳琴.2012.鄂尔多斯盆地晚古生代沉积岩源区构造背景及物源分析.地质学报,86(7):1150-1162.[Chen Q H,Li W H,Hu X L,Li K Y,Pang JG,Guo Y Q.2012.Tectonic setting and provenance analysis of late Paleozoic sedimentary rocks in the Ordos Basin.Acta Geologica Sinica,86(7):1150-1162]
陈全红,李文厚,王亚红,金栓联,高永祥.2006.鄂尔多斯盆地西南部晚古生代早-中期物源分析.现代地质,20(4):628-634.[Chen Q H,Li W H,Wang Y H,Jin S L,Gao Y X.2006.The analysis of sediment provenance in early-middle period of Late Paleozoic in the southwest of Ordos Basin.Geoscience,20(4):628-634]
胡见义,黄第藩.1991.中国陆相石油地质理论基础.北京:石油工业出版社,98-105.[Hu J Y,Huang D F.1991.The Chinese Terrestrial Petroleum Geology Theory Foundation.Beijing:Petroleum Industry Press,98-105]
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王超勇,陈孟晋,汪泽成,郭英海.2007.鄂尔多斯盆地南部二叠系山西组及下石盒子组盒8段沉积相.古地理学报,9(4):369-378.[Wang C Y,Chen M J,Wang Z C,Guo Y H.2007.Sedimentary facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in southern Ordos Basin.Journal of Palaeogeography(Chinese Edition)),9(4):369-378]
王道富,杨华,付进华.2005.鄂尔多斯盆地天然气勘探开发战略研讨.天然气工业,25(4):1-4.[Wang D F,Yang H,Fu J H.2005.Expanding strategy of natural gas exploration and development in Ordos Basin.Natural Gas Industry,25(4):1-4]
王洪亮,肖绍文,徐学义,李万忠,何世平,陈隽璐,陈亮.2008.北秦岭西段吕梁期构造岩浆事件的年代学及其构造意义.地质通报,27(10):1728-1738.[Wang H L,Xiao S W,Xu X Y,Li W Z,He S P,Chen J L,Chen L.2008.Geochronology and significance of the early Mesoproterozoic tectono-magmatic event in the western segment of the North Qinling Mountains,China.Geological Bulletin of China,27(10):1728-1738]
王璇,罗顺社,王睿,李峻颉,王红伟,刘宝宪,段长江.2014.鄂尔多斯盆地三角洲沉积体系及演化规律:以西南部二叠系山1、盒8段为例.科学技术与工程,14(31):25-31.[Wang X,Luo S S,Wang R,Li J J,Wang H W,Liu B X,Duan C J.2014.Delta sedimentary system and evolution of Ordos Basin:With the example of the southwest region of Shan1 and He8 Members,Permian.Science Technology and Engineering,14(31):25-31]
武法东,陈钟惠,张守良,葛立刚.1995.华北石炭二叠纪的海侵作用.现代地质,9(3):284-291.[Wu F D,Chen Z H,Zhang S L,Ge LG.1995.The transgression of Carboniferous and Permian in north China.Geoscience,9(3):284-291]
肖建新,孙粉锦,何乃祥,刘锐娥,李靖,肖红平,张春林.2008.鄂尔多斯盆地二叠系山西组及下石盒子组盒8段南北物源沉积汇水区与古地理.古地理学报,10(4):341-354.[Xiao J X,Sun F J,He N X,Liu R E,Li J,Xiao H P,Zhang C L.2008.Permian Shanxi Formation and Member 8 of Xiashihezi Formation in Ordos Basin:Palaeogeography and catchment area for sediments derived from north and south provenance.Journal of Palaeogeography(Chinese E-dition),10(4):341-354]
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(1)数据据长庆油田。