Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province

The Xinliaodong copper-polymetallic deposit of Eastern Guangdong Province is one of newly discovered deposits. The ore district belongs to tin, tungsten, and copper ore cluster in the southeast coast, which have a very good ore-forming geological conditions. Chalcopyrite has δ65Cu value ranging from...

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Main Authors: FAN Fei-peng, XIAO Hui-liang, CHEN Le-zhu, LI Hai-li, LIU Jian-xiong, DENG Zhong-lin, LI Shao-bin, LIN Geng-wei, ZHOU Xia
Format: Article
Language:English
Published: Science Press, PR China 2017-04-01
Series:Yankuang ceshi
Subjects:
Online Access:http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.201609010133
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author FAN Fei-peng
XIAO Hui-liang
CHEN Le-zhu
LI Hai-li
LIU Jian-xiong
DENG Zhong-lin
LI Shao-bin
LIN Geng-wei
ZHOU Xia
author_facet FAN Fei-peng
XIAO Hui-liang
CHEN Le-zhu
LI Hai-li
LIU Jian-xiong
DENG Zhong-lin
LI Shao-bin
LIN Geng-wei
ZHOU Xia
author_sort FAN Fei-peng
collection DOAJ
description The Xinliaodong copper-polymetallic deposit of Eastern Guangdong Province is one of newly discovered deposits. The ore district belongs to tin, tungsten, and copper ore cluster in the southeast coast, which have a very good ore-forming geological conditions. Chalcopyrite has δ65Cu value ranging from-0.34‰ to +1.37‰, which is consistent with δ65Cu value of porphyry deposits, indicating that ore-forming material Cu was derived from deep magma and ore-forming fluids were medium-high-temperature (250-420℃) magmatic-hydrothermal fluids. There is a close relationship between the fractionation of Cu isotope and magmatic hydrothermal activity. The formation of ore body is related to the dissolution of ore-forming fluids. With the increase of depth, there is atrend of increasing δ65Cu value, indicating a potential of a largee orebody. Copper isotope can directly indicate the location of the heat source. The δ65Cu values are below 0 for copper ore bodies close to the hydrothermal quartz veins.But the copper isotope values are higher in the hydrothermal contact zone, special ore-bearing surrounding rock and tectonic zone where indicates the edge or the front of the main ore body, most obvious ore prospecting mark.
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spelling doaj.art-d74cd60f1d8e4492894eb41bbe93acc62023-02-09T00:48:43ZengScience Press, PR ChinaYankuang ceshi0254-53572017-04-0136442042910.15898/j.cnki.11-2131/td.201609010133ykcs-36-4-420Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong ProvinceFAN Fei-peng0XIAO Hui-liang1CHEN Le-zhu2LI Hai-li3LIU Jian-xiong4DENG Zhong-lin5LI Shao-bin6LIN Geng-wei7ZHOU Xia8Nanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, ChinaNanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, ChinaNanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, ChinaNanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, ChinaFoshan Geological Bureau of Guangdong Province, Foshan 528000, ChinaFoshan Geological Bureau of Guangdong Province, Foshan 528000, ChinaNo.2 Geological Party, Guangdong Geological Bureau, Shantou 515000, ChinaNo.2 Geological Party, Guangdong Geological Bureau, Shantou 515000, ChinaNo.2 Geological Party, Guangdong Geological Bureau, Shantou 515000, ChinaThe Xinliaodong copper-polymetallic deposit of Eastern Guangdong Province is one of newly discovered deposits. The ore district belongs to tin, tungsten, and copper ore cluster in the southeast coast, which have a very good ore-forming geological conditions. Chalcopyrite has δ65Cu value ranging from-0.34‰ to +1.37‰, which is consistent with δ65Cu value of porphyry deposits, indicating that ore-forming material Cu was derived from deep magma and ore-forming fluids were medium-high-temperature (250-420℃) magmatic-hydrothermal fluids. There is a close relationship between the fractionation of Cu isotope and magmatic hydrothermal activity. The formation of ore body is related to the dissolution of ore-forming fluids. With the increase of depth, there is atrend of increasing δ65Cu value, indicating a potential of a largee orebody. Copper isotope can directly indicate the location of the heat source. The δ65Cu values are below 0 for copper ore bodies close to the hydrothermal quartz veins.But the copper isotope values are higher in the hydrothermal contact zone, special ore-bearing surrounding rock and tectonic zone where indicates the edge or the front of the main ore body, most obvious ore prospecting mark.http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.201609010133copper isotopeeastern guangdong provincexinliaodong copper-polymetallic ore districtcopper orebodymagma
spellingShingle FAN Fei-peng
XIAO Hui-liang
CHEN Le-zhu
LI Hai-li
LIU Jian-xiong
DENG Zhong-lin
LI Shao-bin
LIN Geng-wei
ZHOU Xia
Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
Yankuang ceshi
copper isotope
eastern guangdong province
xinliaodong copper-polymetallic ore district
copper orebody
magma
title Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
title_full Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
title_fullStr Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
title_full_unstemmed Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
title_short Copper Isotope Studies of a Deep Ore Body in the Xinliaodong Copper-Polymetallic Deposit, Eastern Guangdong Province
title_sort copper isotope studies of a deep ore body in the xinliaodong copper polymetallic deposit eastern guangdong province
topic copper isotope
eastern guangdong province
xinliaodong copper-polymetallic ore district
copper orebody
magma
url http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.201609010133
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