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Metallogenic discrimination by sphalerite trace element

The Nanmushu Zn Pb deposit is a large scale and representative deposit in the Mayuan ore field on the northern margin of the Yangtze Block This study investigates the trace element geochemistry

Ore forming process of the Huize super large Pb Zn deposit SW China

The Sichuan Yunnan Guizhou SYG Pb Zn metallogenic province is located on the southwestern margin of the Yangtze Block with a complex geological environment and superior metallogenic conditions Han et al 2014 The SYG district is an important component of the low temperature metallogenic domain of South China Hu et al 2017 The SYG district

Genesis of the Bafangshan Erlihe Zn Pb Cu deposit in the

The Fengxian Taibai abbr Fengtai ore cluster in the west Qinling orogen Shaanxi central China comprises an important part of the giant Qinling Zn Pb Au metallogenic belt Fig 1 a and b The total Pb Zn reserve is >5 Mt with a Au reserve of >200 t in the ore cluster Wang et al 2007 Li 2008 In the Fengtai ore cluster there are three large Zn Pb Cu

Timing and origin of multi stage magmatism and related W Mo Pb Zn Fe Cu

The Tongshanling ore field is one of the most representative W Sn Cu Pb Zn polymetallic deposits in the central western Nanling Ore Belt which developed multiple mineralization types

PDF Discrimination of Pb Zn deposit types using sphalerite

A dataset of nearly 3600 sphalerite spot analyses from 95 Pb Zn deposits worldwide determined by LA ICP MS was compiled from peer reviewed publications containing 12 elements Mn Fe Co Cu Ga

Trace element geochemistry and O S Pb He Ar isotopic

The Jiangnan Orogenic Belt is an important polymetallic metallogenic belt in South China rich in Au Sb W Cu Co Pb and Zn and even Nb and Ta resources Deng et al 2017a Hu and Peng 2018 Wang et al 2017 Xiong et al 2020a Xiong et al 2020b Xu et al 2017a Zhou et al 2019 Zou et al 2018 geochemistry and ore genesis

Ore genesis and tectonic setting of the Bieluwutu Cu Pb Zn

The Bieluwutu Cu Pb Zn deposit is located in the Ondor Sum region of the western Xing an Mongolia orogenic belt North China The host rocks of the deposit consist of metasandstone tuffaceous

Porphyry Cu Au Mo epithermal Ag Pb Zn distal

Request PDF Porphyry Cu Au Mo epithermal Ag Pb Zn distal hydrothermal Au deposits in the Dexing area Jiangxi province East China A linked ore system Based on previous studies and detailed

Origin of ore forming fluids of the Zn Pb Cu deposits in

Request PDF Origin of ore forming fluids of the Zn Pb Cu deposits in the Jinbao mine district of eastern Guizhou Province China Evidence from chemical compositions of fluid inclusions and

Textures trace elements and Pb isotopes of sulfides from

The Haopinggou deposit in the Xiong ershan district southern margin of the North China Craton comprises numerous Au and Ag Pb Zn veins hosted in metamorphic rocks of the Late Archean to early Paleoproterozoic Taihua Group Two stages of mineralization have been recognized Stage 1 pyrite quartz veins and Stage 2 Pb Zn sulfide veins Some

Ore forming conditions and genesis of the Huogeqi Cu Pb Zn…

DOI / Corpus ID 128956720; Ore forming conditions and genesis of the Huogeqi Cu Pb Zn Fe deposit in the northern margin of the North China Craton Evidence from ore petrologic characteristics

Frontiers 3D mineral exploration Cu Zn

The Tiemurt Pb Zn Cu deposit metal reserve Mt Pb Zn and Mt Cu is hosted in the Kangbutiebao Formation volcanic sedimentary rocks in the Chinese Altay Orogen NW China

Pyrite geochemical fingerprinting on skarn ore forming

Pyrite geochemistry has been extensively used to reveal ore forming processes in diverse ore deposits but its application in skarn systems is not well understood The Huangshaping deposit in the Nanling Range South China uniquely develops W Sn Pb Zn and Cu Pb Zn skarn mineralization systems and both two systems have formed multi types of

Genesis of the Huangtupo Cu Zn deposit Eastern Tianshan NW China

Huangtan Au Cu Zn is an auriferous VMS deposit hosted in tuff breccia and tuff of Silurian age in the Kalatag area that located in the northern part of East Tianshan

Insights into ore genesis of the Beishan Pb Zn deposit in

The Beishan Pb Zn deposit is located 47 km northwest of Huanjiang County north of Hechi City Guangxi Fig 1 a b and includes several mineralized occurrences developed in mining areas such as Shangchao Huada and Beishan Pb Zn deposit has a history of discovering native siderite when searching for Fe mineralization and then

Middle Triassic Cu Pb Zn Skarn mineralization in the Wulonggou gold ore

DOI / Corpus ID 270768975; Middle Triassic Cu Pb Zn Skarn mineralization in the Wulonggou gold ore field Eastern Kunlun Orogen NW China Insights from phlogopite Ar Ar and zircon U Pb dating and Sr Nd Pb Hf isotopes

Contrasting regimes of Cu Zn and Pb transport in ore

Request PDF On Feb 1 2015 Richen Zhong and others published Contrasting regimes of Cu Zn and Pb transport in ore forming hydrothermal fluids Find read and cite all the research you need on

Genesis of Pb&ndash;Zn Mineralization in the Pulang Cu

The Pulang super large porphyry Cu polymetallic deposit located in the Sanjiang area of Yunnan Province is one of the largest Cu deposits in China This deposit hosts Cu resources of 5 × 106 t and other ore forming elements such as Mo Au Ag Pb Zn Pt and Pd Recently obvious hydrothermal vein type Pb Zn mineralization with a Pb Zn resource of

LA ICP MS trace element analysis of sphalerite and

The Beishan Pb Zn ore district located in northern Guangxi China is a giant carbonate hosted Pb Zn ore district In situ trace element analysis was performed using LA ICP MS on sphalerite and

[PDF] Porphyry Cu Au Mo epithermal Ag Pb Zn distal

Semantic Scholar extracted view of "Porphyry Cu Au Mo epithermal Ag Pb Zn distal hydrothermal Au deposits in the Dexing area Jiangxi province East China—A linked ore system" by J Mao et al The Jinshan gold deposit a superlarge deposit with 200 t Au is hosted in the Jinshan ductile shear zone and located in the northeast

A Preliminary Review on the Metallogeny of

The Qin Hang ore belt in South China which serves as the boundary between the Yangtze and Cathaysia blocks is marked by extensive Jurassic porphyry skarn metasomatic Cu Pb Zn polymetallic

Re Os and U Pb geochronology of the Laochang Pb Zn

Pyrite grains in textural equilibrium with galena sphalerite and chalcopyrite from stratabound Pb Zn Ag and Cu bearing Pb Zn Ag orebodies have a Re Os isochron age of ± Ma

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