新疆若羌县红柳沟Ⅰ号剖面新元古界成冰系冰沟南组硅质岩特征与沉积环境  

Characteristics and sedimentary environment of siliceous rock in the Neoproterozoic Cryogenian Binggounan Formation at Hongliugou sectionⅠin Ruoqiang County,Xinjiang

作　　者：钱一雄[1] 李曰俊[2] 储呈林 杨鑫[3] 李王鹏 陈跃[1] 马红强[1] Qian Yi-Xiong;Li Yue-Jun;Chu Cheng-Lin;Yang Xin;Li Wang-Peng;Chen Yue;Ma Hong-Qiang(Wuxi Inusirute,Exploration&Prodaction Reearch Insiude,SINOPEC,Jiangsu Wuxi 214151,China;Instiute of Geology and Geophysir,Chimee Acrdemy of Sciences,Beijing 100029,China;Exploration&Prodution Research Istitute,SINOPEC,Beijing 10083,China)

机构地区：[1]中国石化石油勘探开发研究院无锡石油地质研究所,江苏无锡214151 [2]中国科学院地质与地球物理研究所,北京100029 [3]中国石化石油勘探开发研究院,北京100083

出　　处：《古地理学报》2021年第4期668-682,共15页Journal of Palaeogeography：Chinese Edition

基　　金：国家深地项目“中新元古界微生物碳酸盐岩沉积环境与成储机制”(编号:2017YFC0603103);中国石化项目“塔里木盆地新元古界-寒武系沉积特征与源储条件”(编号:P17046-4)联合资助。

摘　　要：新疆若羌县红柳沟Ⅰ号剖面出露厚约300 m的新元古界成冰系冰沟南组的细粒沉积物和碳酸盐岩等,并发现有沥青油气显示。通过厚160 m左右硅质岩剖面实测以及岩石学、地球化学等研究表明:红柳沟Ⅰ号剖面中的硅质岩主要由石英、黏土构成,有微量的含铁、锰、磷的独立矿物;具有隐晶质、微晶石英和粗—巨晶石英"镶嵌结构"3种结构类型;硅质岩中SiO_(2)、Fe_(2)O_(3)、Ba和δEu_(n)值相对较高,Al_(2)O_(3)、MnO、MnO/TiO_(2)、U/Th和Sr/Ba值较低,ΣREE、Sr/Ba、MnO_(2)/TiO_(2)和δCe_(n)值等呈现有规律的变化;δ^(30)Si值平均为-0.43‰(-0.8‰~0.3‰),δ^(18)O_(Snow)值平均为20.42‰(16.0‰~26.0‰),估算的平均温度为90℃(52~127℃),指示了硅质岩具有多个沉积旋回,在海水与热水参与的大陆边缘盆地中沉积,并经历了早成岩期、浅埋藏期以及与多期走滑断裂活动有关的热流体与大气淡水的叠加改造。The fine-grained sediments and carbonate rocks with a thickness of 300 m are discovered at the Binggounan Formation of Neoproterozoic Cryogenian system in Hongliugou sectionⅠof Altyn in Xinjiang,and the asphalt which is the indicator of oil and gas is also found.Based on the section measurement,petrology and geochemistry of the 160 m thickness of siliceous rocks,it shows that siliceous rocks in the profile are mainly composed of quartz,clay,and tiny amounts of iron,manganese and phosphorusbearing independent minerals.It has three types of structures,including cryptocrystalline,microcrystalline quartz and coarse-megacrystalline quartz with a"mosaic structure".The concents of SiO_(2),Fe_(2)O_(3),Ba andδEu_(n)in siliceous rocks are relatively high,while the contents of Al2 O_(3),MnO,MnO/Ti O_(2),U/Th,Sr/Ba are much lower.The values ofΣREE,Sr/Ba,MnO_(2)/Ti O_(2)andδCe_(n)change regularly.The averageδ^(30)Si is-0.43‰(-0.8‰~0.3‰),and the averageδ18 O_(Snow)is 20.42‰(16.0‰~26.0‰),and the estimated average temperature is 90℃(52~127℃),which indicates that there are multiple sedimentary cycles for the siliceous rocks.They deposit in the continental margin basin that is characterized as the mixing of sea water and hydrothermal fluid.Afterwards,they underwent the early diagenesis,shallow burial period,the superimposition and reworking of thermal and fresh water related with the multiple strike slipping activities.

关 键 词：硅质岩 岩石学 地球化学 新元古界 阿尔金断裂 若羌县 

分 类 号：P588.2[天文地球—岩石学]