滇东南丘北地区上二叠统吴家坪阶硅质岩地球化学特征及地质意义  

Geochemical Feature of Upper Permian Wuchiapingian Cherts of Qiubei Region,Southeast Yunnan and Its Geological Significance

作　　者：刘加强[1] 王训练[1] 周洪瑞[1] 高金汉[1] 于蕾[1] 毛志芳[1] 郑楠[1] 

机构地区：[1]中国地质大学(北京)地球科学与资源学院,北京100083

出　　处：《沉积学报》2013年第4期621-629,共9页Acta Sedimentologica Sinica

基　　金：中国地质调查局项目"不同地层区地层系统的完善与对比研究"(编号:基[20l1]01-47-09)资助

摘　　要：运用岩石学和地球化学的方法研究滇东南丘北地区晚二叠世吴家坪期硅质岩,取得以下主要认识:(1)滇东南丘北地区硅质岩SiO2/Al2O3值除样品P29外均大于80,Al/(Al+Fe+Mn)为0.46～0.76,表明硅质岩主要为生物成因,受陆源碎屑影响较小;(2)硅质岩Ce/Ce*为0.517～0.858,LaN/CeN为1.12～1.80,经球粒陨石标准化的稀土模式则表现为轻稀土元素富集,且具有明显负Eu异常的右倾型,表明沉积环境为大陆边缘;(3)样品P29硅质岩Eu/Eu*为1.129,反映其受到一定程度热液的影响,可能受峨眉山地幔柱或(和)断裂的共同影响。Cherts of the Late Permian occurred extensively in the Dian-Qian-Gui region,which provide critical information with respect to the study of tectonic setting and the formation of sedimentary basins.At present most attention has been focused on Guangxi and Southwestern Guizhou,however,few relevant research has been carried out in Southeast Yunnan.Based on petrogeology and geochemistry,the Wuchiapingian cherts of Upper Permian of Qiubei region,Southeast Yunnan have been systematically studied.The results show that all samples except P29 have much higher SiO2/ Al2O3 ratios（ 80）,Al /（Al ＋ Fe ＋ Mn） ratio between 0.46 and 0.76;Ce / Ce＊ and LaN/ CeNratios are 0.517 ～ 0.858 and 1.12 ～ 1.80,respectively;Chondrite-normalized REE patterns of the cherts characterized by significant negative Eu anomalies and LREE enrichment;Besides,the NASC-normalized Eu / Eu＊ ratio of P29 is 1.129.Combining with the published geochemical data of cherts from the equivalent horizons of Dongpan and Laibin region,we draw a conclusion that（1） The cherts of Qiubei and Dongpan region developed in a setting of continental marginal in the late Permian,and terrestrial debris is the main material source of the cherts of Dongpan.Meanwhile,the cherts of Qiubei are characteristic of biogenesis,and received little terrigenous input,and those of Laibin were deposited in an ocean basin with influence of submarine hydrothermal fluid and no input of terrigenous materials;the Eu / Eu＊ ratio of P29 is 1.129,which reflects its hydrothermal influence and implies the movement from both（either） Emeishan Mantle and（or） regional fault;During the late Permian,the water depth of Qiubei region deepen gradually from west to east with low water energy.

关 键 词：滇东南丘北地区 上二叠统吴家坪阶 硅质岩 地球化学特征 

分 类 号：P534.63[天文地球—第四纪地质学] P595[天文地球—古生物学与地层学]