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The Qin Hang porphyry skarn copper polymetallic ore belt QHB is located along a significant NE SW trending Neoproterozoic suture in South China which separates the Yangtze Craton and Cathaysian Blocks Fig 1a; Mao et al 2011a containing several large and super large W Sn Cu Au Pb Zn Ag and polymetallic QHB is approximately
Metal pollution in urban soils due to smelting and electroplating has become a severe problem in China In this study the concentration chemical fraction and leaching behavior of typical metals Cu Zn Cd and Pb in soil samples from ten metallurgical sites were studied The results show that some of the soils were polluted with Cu and most were heavily polluted
Because lead smelting does not result in obvious accumulation of Cu and Zn in the environment Basta and Gradwohl 2000; Ran et al 2010; Cheng et al 2014 the higher IBAF values of Cu and Zn in this work may be due to the fact that the proportion of these two elements from smelting activities is lower than those of Pb and Cd thus the
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
Nevertheless some important Pb Zn polymetallic deposits linked to the Late Jurassic Early Cretaceous granitoids and/or coeval intermediate to felsic volcanic and subvolcanic rocks have also been discovered in the Jiangnan Au Cu Pb Zn Sb Ag W metallogenic belt Xu et al 2017a Xu et al 2017b the Jurassic Qin Hang Qinzhou Hangzhou
To that end the sorption and transport of five metals—Cr Pb Cd Cu and Zn—was evaluated using representative samples of a soil from the north of Portugal The tests were conducted in batch and continuous systems using single and multiple metal acid solutions to evaluate the effect of metal competition Several representative soil
The Kalatag area located in the middle of the Harlik Dananhu arc in East Tianshan orogen hosts several Cu Zn deposits including the Huangtupo VMS Cu Zn deposit including the Honghai deposit and the Hongshan Hongshi and Meiling hydrothermal lode type Cu deposits Figs 1 C and 2; Fang et al 2002 Mao et al 2010 Deng et al
Selenium Sb Te and Au of Py1b are mostly below the detection limits Py1b shows lower Cu Zn As Ag and Bi contents than Py1b with mean values of 1550 4940 2870 and ppm respectively Lead contents of Py1b vary between and 30 500 ppm Some analyses with outliers of Cu Zn As and Pb may include some micro inclusions
The small scale Balugou Cu Pb Zn skarn deposit 45 298 tonnages of ore at % to % Cu % to % Pb and % to % Zn is located in the Wulonggou area in the eastern Kunlun orogen NW China Ore deposition is spatially and temporally related with the pre collisional Anisian Balugou granites 244 Ma The mineralization hosted by the
On an ore field scale some Cordilleran Cu bearing mineralization is thought to be part of a porphyry Cu system An example is the Zn Pb Ag Cu Bi mineralization at Cerro de Pasco and Cu Zn Pb Au Ag mineralization in the Colquijirca district of Peru which are thought to be located in the upper parts of Cu bearing porphyries
Geochemical mapping is an important tool in both mineral exploration and environmental studies Grunsky et al 2009 China s National Geochemical Mapping Project Regional Geochemistry National Reconnaissance was initiated in 1979 Xie et al 1997 and has covered more than 6 million km 2 of China s territory Xie et al 2008 This project
The averages are for Mn for Fe for Co 14 for Ni 138 for Cu 106 for Zn 581 for Cd and 155 for Pb They suggested that Cu Zn Cd and Pb are primarily of anthropogenic origin EF dPb in the ECS is of the same order of magnitude as the EF Pb in the ECS atmospheric aerosol These results suggest that dPb is derived from
The Yinshan Cu Au Pb Zn Ag deposit is located in the famous Dexing copper gold polymetallic district in South China Fig 1 This polymetallic district consists of the Middle Jurassic ca 170 Ma Yinshan Cu Au Pb Zn Ag deposit 950 000 tons of Cu and 107 tons of Au JGEB 1996 Yinshan Lead Zinc Mine 1993 Wang et al 2011b the Middle
Cargas asociadas Pb Zn Cu Cd y Cr La fracción de tamaño < 63 μm tendió a asociar el mayor porcentaje de carga de metales pesados %/kg de sedimento ó %/m 2 ver tabla 5 Excepto para Pb y Cu donde la fracción de tamaño con mayor contenido de elementos metálicos fue entre 250 500 μm El aumento de la carga asociada de
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
Unlike Cr Cu Cd and Pb the maximum Zn concentration was not found in plants at site HN 4 or HN 5 but in A philoxeroides 365 mg kg −1 at site HN 3 Furthermore Z candida and C dactylon at site HN 2 and even C rotundus at Site HN 6 contained Zn concentrations greater than 200 mg kg −1 exceeding the highest Zn concentration of
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The Dachang tin polymetallic district Guangxi China is one of the largest tin ore fields in the world Both cassiterite sulfide and Zn Cu skarn mineralization are hosted in the Mid Upper Devonian carbonate rich sediments adjacent to the underlying Cretaceous Longxianggai granite 91 97 Ma The Lamo Zn Cu deposit is a typical skarn deposit in the
1 Introduction Lakes are important and significant bodies in preserving freshwater and replenishing underground water also act as a key role in adjusting local climate and ameliorating environment consequently they are considered one of the most versatile ecosystems in the world Forghani et al 2009 Hu et al 2012 China has about 2848 lakes
The Jinding Zn Pb deposit located in the Mesozoic Cenozoic Lanping Basin of southwest China has ore reserves of ∼ 220 Mt with an average grade of % Zn and % mineralization is hosted by sandstone in the Early Cretaceous Jingxing Formation and limestone breccia in the Paleocene Yunlong Formation
The southeastern coastal metallogenic belt hereinafter referred to as SCMB where Mesozoic igneous rocks are widely exposed and accompanied by large scale W Sn Cu Mo Pb Zn Au Ag polymetallic mineralization of Mesozoic age is an important part of the Circum Pacific metallogenic belts Mao et al 2018 The central Fujian region hereafter referred to as
Jinchanghe is a Zn Pb Fe Cu skarn deposit in the northern Baoshan block southwestern China It is a typical distal skarn deposit with orebodies in the Cambrian Hetaoping Formation limestone and calcareous siltstone The skarn minerals display a vertical zonation with garnet skarn in the lower part and pyroxene skarn in the upper part Economic metals are also