首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Cryptic sediment-hosted critical element mineralization from eastern Yunnan Province, southwestern China: Mineralogy, geochemistry, relationship to Emeishan alkaline magmatism and possible origin
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Cryptic sediment-hosted critical element mineralization from eastern Yunnan Province, southwestern China: Mineralogy, geochemistry, relationship to Emeishan alkaline magmatism and possible origin

机译:中国西南部云南东部隐匿性沉积物的关键元素矿化作用:矿物学,地球化学,与峨眉山碱性岩浆作用的关系及其可能成因

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A previous study briefly described the occurrence of a new type of Nb(Ta)-Zr(Hf)-REY-Ga (REY: rare earth elements and yttrium) polymetallic mineralization in eastern Yunnan, southwest China. In this paper, the mineralogical and geochemical features have been further advanced through a study of two regionally extensive and relatively flat-lying mineralized layers from No. XW drill core. The layers are clay-altered volcanic ash and tuffaceous clay, and are dominated by clay minerals (mixed layer illite/smectite, kaolinite, berthierine, and chamosite); with lesser amounts of quartz and variable amounts of anatase, siderite and calcite; along with trace pyrite, barite, zircon, ilmenite, galena, chalcopyrite, and REE-bearing minerals. The mineralized samples have higher Al2O3/TiO2 values (13.7-41.4) and abundant rare metal elements (Nb, Ta, Zr, Hf, REE, Ga, Th, and U) whereas less mineralized samples are rich in V, Cr, Co, and Ni and have lower Al2O3/TiO2 values (2.32-7.67). The mineralized samples also have strong negative delta Eu in chondrite-normalized REE patterns. Two processes are most likely responsible for the geochemical and mineralogical anomalies of the mineralized samples: airborne volcanic ash and multi-stage injection of low-temperature hydrothermal fluids. Based on paragenetic analysis, this polymetallic mineralization is derived from the interaction between alkaline volcanic ashes and subsequent percolation of low-temperature fluids. The intense and extensive alkaline volcanism of the early Late Permian inferred from this study possibly originated from the coeval Emeishan large igneous province (ELIP). This unique Nb(Ta)-Zr(Hf)-REE-Ga mineralization style has significant economic and geological potential for the study of mineralization of the lowest Xuanwei Formation. (C) 2016 Elsevier B.V. All rights reserved.
机译:先前的研究简要描述了在中国西南云南东部发生的一种新型的Nb(Ta)-Zr(Hf)-REY-Ga(REY:稀土元素和钇)多金属矿化现象。在本文中,通过对XW号钻芯的两个区域广泛且相对平坦的矿化层进行了研究,进一步提高了矿物学和地球化学特征。这些层是改变了粘土的火山灰和凝灰质粘土,并且以粘土矿物(伊利石/蒙脱石,高岭石,白屈菜碱和硅铁矿的混合层)为主。较少量的石英和少量的锐钛矿,菱铁矿和方解石;以及微量的黄铁矿,重晶石,锆石,钛铁矿,方铅矿,黄铜矿和含REE的矿物。矿化样品具有较高的Al2O3 / TiO2值(13.7-41.4)和丰富的稀有金属元素(Nb,Ta,Zr,Hf,REE,Ga,Th和U),而矿化程度较低的样品富含V,Cr,Co,和Ni并具有较低的Al2O3 / TiO2值(2.32-7.67)。矿化样品在球粒晶归一化REE模式中也具有很强的负δEu。矿化样品的地球化学和矿物学异常可能是由以下两个过程引起的:机载火山灰和低温热液的多阶段注入。基于共生分析,这种多金属矿化作用是由碱性火山灰和随后的低温流体渗滤之间的相互作用引起的。根据这项研究推断,晚二叠纪强烈而广泛的碱性火山活动可能起源于中世纪的峨眉山大火成岩省(ELIP)。这种独特的Nb(Ta)-Zr(Hf)-REE-Ga矿化方式对于研究最低宣威组的矿化具有重要的经济和地质潜力。 (C)2016 Elsevier B.V.保留所有权利。

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