典型文献
Multiple-Stage Mineralization in the Huayangchuan U-REE-Mo-Cu-Fe Ore Belt of the Qinling Orogen, Central China:Geological and Re-Os Geochronological Constraints
文献摘要:
The Huayangchuan ore belt is located in the western segment of Xiaoqinling Orogen in the southern margin of the North China Craton (NCC), and hosts voluminous magmatism and signifi- cant U-REE-Mo-Cu-Fe polymetallic mineralization. However, geochronological framework of the vari- ous mineralization phases in this region is poorly understood. Here, we present new Re-Os isochron ag- es on magnetite from the Caotan Fe deposit (2675 ± 410 Ma, MSWD=0.55), and on pyrite from the Jialu REE deposit (2127 ± 280 Ma, MSWD=1.9) and Yuejiawa Cu deposit (418 ± 23 Ma, MSWD= 11.5), and Re-Os weighted average model age on pyrite from the Taoyuan Mo-U deposit (235 ± 14 Ma, MSWD=0.17). These ages, combined with regional geology and mineralization ages from other depos- its, suggest that mineralization in the Huayangchuan ore belt lasted from the Neoarchean to the Late Mesozoic. The mineralization corresponds to regional tectono-magmatic events, including the Neoar- chean alkali magmatism (REE mineralization), Paleoproterozoic plagioclase-amphibolite emplacement (Fe mineralization), Paleoproterozoic pegmatite magmatism (U mineralization), Paleozoic Shangdan oceanic slab subduction-related arc magmatism (Cu mineralization), Early Mesozoic Paleo-Tethys Ocean subduction-related arc magmatism (Mo-U mineralization), and Late Mesozoic Paleo-Pacific oce- anic plate subduction direction change-related Mo(-Pb) mineralization. We proposed that the Huayang- chuan ore belt has undergone prolonged metallogenic evolution, and the magmatism and associated mineralization were controlled by regional geodynamic events.
文献关键词:
中图分类号:
作者姓名:
Hongjun Jiang;Chunsi Yang;Dequan Wang;Hui Zheng;Jie Li;Huayong Chen
作者机构:
Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;University of Chinese Academy of Sciences,Beijing 100049,China;Geological Party No.214,Sino Shaanxi Nuclear Industry Group,Xi'an 710100,China;Sino Shaanxi Nuclear Industry Group,Xi'an 710100,China;State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;CAS Center for Excellence in Deep Earth Science,Guangzhou 510640,China;Guangdong Provincial Key Laboratory of Mineral Physics and Materials,Guangzhou 510640,China
文献出处:
引用格式:
[1]Hongjun Jiang;Chunsi Yang;Dequan Wang;Hui Zheng;Jie Li;Huayong Chen-.Multiple-Stage Mineralization in the Huayangchuan U-REE-Mo-Cu-Fe Ore Belt of the Qinling Orogen, Central China:Geological and Re-Os Geochronological Constraints)[J].地球科学学刊(英文版),2022(01):193-204
A类:
Huayangchuan,Xiaoqinling,Caotan,Jialu,Yuejiawa,Taoyuan,Neoar,chean,Shangdan,oce,anic,Huayang,chuan
B类:
Multiple,Stage,Mineralization,REE,Mo,Ore,Belt,Qinling,Orogen,Central,China,Geological,Re,Os,Geochronological,Constraints,ore,belt,located,western,segment,southern,margin,North,Craton,NCC,hosts,voluminous,magmatism,signifi,cant,polymetallic,mineralization,However,geochronological,framework,vari,phases,this,poorly,understood,Here,present,new,isochron,magnetite,from,deposit,Ma,MSWD,pyrite,weighted,average,model,These,ages,combined,regional,geology,other,its,suggest,that,lasted,Neoarchean,Late,Mesozoic,corresponds,tectono,magmatic,events,including,alkali,Paleoproterozoic,plagioclase,amphibolite,emplacement,pegmatite,Paleozoic,oceanic,slab,subduction,related,Early,Tethys,Ocean,Pacific,plate,direction,change,Pb,We,proposed,undergone,prolonged,metallogenic,evolution,associated,were,controlled,by,geodynamic
AB值:
0.466588
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