Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes

Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz vei...
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Gespeichert in:

Autor*in:	Yin, Hejun [verfasserIn] Huang, Jianguo Ren, Tao

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Badi copper deposit Fluid inclusion Sulfur isotope Hydrogen and oxygen isotope Ore genesis

Anmerkung:	© Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017

Übergeordnetes Werk:	Enthalten in: Chinese journal of geochemistry - Beijing : Science Press, 1982, 37(2017), 4 vom: 25. Nov., Seite 559-570
Übergeordnetes Werk:	volume:37 ; year:2017 ; number:4 ; day:25 ; month:11 ; pages:559-570

Links:	Volltext

DOI / URN:	10.1007/s11631-017-0252-5

Katalog-ID:	SPR021279799

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520			\|a Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit.
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allfields	10.1007/s11631-017-0252-5 doi (DE-627)SPR021279799 (SPR)s11631-017-0252-5-e DE-627 ger DE-627 rakwb eng Yin, Hejun verfasserin aut Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017 Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213 Huang, Jianguo aut Ren, Tao aut Enthalten in Chinese journal of geochemistry Beijing : Science Press, 1982 37(2017), 4 vom: 25. Nov., Seite 559-570 (DE-627)341897779 (DE-600)2069518-4 1993-0364 nnns volume:37 year:2017 number:4 day:25 month:11 pages:559-570 https://dx.doi.org/10.1007/s11631-017-0252-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_110 GBV_ILN_152 GBV_ILN_161 GBV_ILN_187 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2700 AR 37 2017 4 25 11 559-570
spelling	10.1007/s11631-017-0252-5 doi (DE-627)SPR021279799 (SPR)s11631-017-0252-5-e DE-627 ger DE-627 rakwb eng Yin, Hejun verfasserin aut Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017 Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213 Huang, Jianguo aut Ren, Tao aut Enthalten in Chinese journal of geochemistry Beijing : Science Press, 1982 37(2017), 4 vom: 25. Nov., Seite 559-570 (DE-627)341897779 (DE-600)2069518-4 1993-0364 nnns volume:37 year:2017 number:4 day:25 month:11 pages:559-570 https://dx.doi.org/10.1007/s11631-017-0252-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_110 GBV_ILN_152 GBV_ILN_161 GBV_ILN_187 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2700 AR 37 2017 4 25 11 559-570
allfields_unstemmed	10.1007/s11631-017-0252-5 doi (DE-627)SPR021279799 (SPR)s11631-017-0252-5-e DE-627 ger DE-627 rakwb eng Yin, Hejun verfasserin aut Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017 Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213 Huang, Jianguo aut Ren, Tao aut Enthalten in Chinese journal of geochemistry Beijing : Science Press, 1982 37(2017), 4 vom: 25. Nov., Seite 559-570 (DE-627)341897779 (DE-600)2069518-4 1993-0364 nnns volume:37 year:2017 number:4 day:25 month:11 pages:559-570 https://dx.doi.org/10.1007/s11631-017-0252-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_110 GBV_ILN_152 GBV_ILN_161 GBV_ILN_187 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2700 AR 37 2017 4 25 11 559-570
allfieldsGer	10.1007/s11631-017-0252-5 doi (DE-627)SPR021279799 (SPR)s11631-017-0252-5-e DE-627 ger DE-627 rakwb eng Yin, Hejun verfasserin aut Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017 Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213 Huang, Jianguo aut Ren, Tao aut Enthalten in Chinese journal of geochemistry Beijing : Science Press, 1982 37(2017), 4 vom: 25. Nov., Seite 559-570 (DE-627)341897779 (DE-600)2069518-4 1993-0364 nnns volume:37 year:2017 number:4 day:25 month:11 pages:559-570 https://dx.doi.org/10.1007/s11631-017-0252-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_110 GBV_ILN_152 GBV_ILN_161 GBV_ILN_187 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2700 AR 37 2017 4 25 11 559-570
allfieldsSound	10.1007/s11631-017-0252-5 doi (DE-627)SPR021279799 (SPR)s11631-017-0252-5-e DE-627 ger DE-627 rakwb eng Yin, Hejun verfasserin aut Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017 Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213 Huang, Jianguo aut Ren, Tao aut Enthalten in Chinese journal of geochemistry Beijing : Science Press, 1982 37(2017), 4 vom: 25. Nov., Seite 559-570 (DE-627)341897779 (DE-600)2069518-4 1993-0364 nnns volume:37 year:2017 number:4 day:25 month:11 pages:559-570 https://dx.doi.org/10.1007/s11631-017-0252-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_110 GBV_ILN_152 GBV_ILN_161 GBV_ILN_187 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2700 AR 37 2017 4 25 11 559-570
language	English
source	Enthalten in Chinese journal of geochemistry 37(2017), 4 vom: 25. Nov., Seite 559-570 volume:37 year:2017 number:4 day:25 month:11 pages:559-570
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author	Yin, Hejun
spellingShingle	Yin, Hejun misc Badi copper deposit misc Fluid inclusion misc Sulfur isotope misc Hydrogen and oxygen isotope misc Ore genesis Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
authorStr	Yin, Hejun
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topic_title	Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes Badi copper deposit (dpeaa)DE-He213 Fluid inclusion (dpeaa)DE-He213 Sulfur isotope (dpeaa)DE-He213 Hydrogen and oxygen isotope (dpeaa)DE-He213 Ore genesis (dpeaa)DE-He213
topic	misc Badi copper deposit misc Fluid inclusion misc Sulfur isotope misc Hydrogen and oxygen isotope misc Ore genesis
topic_unstemmed	misc Badi copper deposit misc Fluid inclusion misc Sulfur isotope misc Hydrogen and oxygen isotope misc Ore genesis
topic_browse	misc Badi copper deposit misc Fluid inclusion misc Sulfur isotope misc Hydrogen and oxygen isotope misc Ore genesis
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title	Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
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title_full	Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
author_sort	Yin, Hejun
journal	Chinese journal of geochemistry
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author_browse	Yin, Hejun Huang, Jianguo Ren, Tao
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author-letter	Yin, Hejun
doi_str_mv	10.1007/s11631-017-0252-5
title_sort	ore genesis of badi copper deposit, northwest yunnan province, china: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
title_auth	Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
abstract	Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017
abstractGer	Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017
abstract_unstemmed	Abstract The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vapor–liquid two-phase fluid inclusions, $ CO_{2} $-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins. Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids: (1) low-temperature, low-salinity fluid; (2) medium-temperature, low salinity $ CO_{2} $-bearing; and (3) high-temperature, Fe-rich, high sulfur fugacity. The $ δ^{18} $O values of chalcopyrite-bearing quartz ranged from 4.96‰ to 5.86‰, with an average of 5.40‰. The δD values of ore-forming fluid in equilibrium with the sulfide-bearing quartz were from − 87‰ to − 107‰, with an average of − 97.86‰. These isotopic features indicate that the ore-forming fluid is a mixing fluid between magmatic fluid and meteoric water. The $ δ^{34} $S values of chalcopyrite ranged from 13.3‰ to 15.5‰, with an average of 14.3‰. Sulfur isotope values suggest that the sulfur in the deposit most likely derived from seawater. Various fluid inclusions coexisted in the samples; similar homogenization temperature to different phases suggests that the Badi fluid inclusions might have been captured under a boiling system. Fluid boiling caused by fault activity could be the main reason for the mineral precipitation in the Badi deposit. © Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017
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title_short	Ore genesis of Badi copper deposit, northwest Yunnan Province, China: evidence from geology, fluid inclusions, and sulfur, hydrogen and oxygen isotopes
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