Re–Os Pyrite Geochronological Evidence of Three Mineralization Styles within the Jinchang Gold Deposit, Yanji–Dongning Metallogenic Belt, Northeast China
The Jinchang gold deposit is located in the eastern Yanji–Dongning Metallogenic Belt in Northeast China. The orebodies of the deposit are hosted within granite, diorite, and granodiorite, and are associated with gold-mineralized breccia pipes, disseminated gold in ores, and fault-controlled gold-bea...
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| Published in | Minerals (Basel) Vol. 8; no. 10; p. 448 |
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| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
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12.10.2018
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| ISSN | 2075-163X 2075-163X |
| DOI | 10.3390/min8100448 |
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| Abstract | The Jinchang gold deposit is located in the eastern Yanji–Dongning Metallogenic Belt in Northeast China. The orebodies of the deposit are hosted within granite, diorite, and granodiorite, and are associated with gold-mineralized breccia pipes, disseminated gold in ores, and fault-controlled gold-bearing veins. Three paragenetic stages were identified: (1) early quartz–pyrite–arsenopyrite (stage 1); (2) quartz–pyrite–chalcopyrite (stage 2); and (3) late quartz–pyrite–galena–sphalerite (stage 3). Gold is hosted predominantly within pyrite. Pyrite separated from quartz–pyrite–arsenopyrite cement within the breccia-hosted ores (Py1) yield a Re–Os isochron age of 102.9 ± 2.7 Ma (MSWD = 0.17). Pyrite crystals from the quartz–pyrite–chalcopyrite veinlets (Py2) yield a Re–Os isochron age of 102.0 ± 3.4 Ma (MSWD = 0.2). Pyrite separated from quartz–pyrite–galena–sphalerite veins (Py3) yield a Re–Os isochron age of 100.9 ± 3.1 Ma (MSWD = 0.019). Re–Os isotopic analyses of the three types of auriferous pyrite suggest that gold mineralization in the Jinchang Deposit occurred at 105.6–97.8 Ma (includes uncertainty). The initial 187Os/188Os values of the pyrites range between 0.04 and 0.60, suggesting that Os in the pyrite crystals was derived from both crust and mantle sources. |
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| AbstractList | The Jinchang gold deposit is located in the eastern Yanji–Dongning Metallogenic Belt in Northeast China. The orebodies of the deposit are hosted within granite, diorite, and granodiorite, and are associated with gold-mineralized breccia pipes, disseminated gold in ores, and fault-controlled gold-bearing veins. Three paragenetic stages were identified: (1) early quartz–pyrite–arsenopyrite (stage 1); (2) quartz–pyrite–chalcopyrite (stage 2); and (3) late quartz–pyrite–galena–sphalerite (stage 3). Gold is hosted predominantly within pyrite. Pyrite separated from quartz–pyrite–arsenopyrite cement within the breccia-hosted ores (Py1) yield a Re–Os isochron age of 102.9 ± 2.7 Ma (MSWD = 0.17). Pyrite crystals from the quartz–pyrite–chalcopyrite veinlets (Py2) yield a Re–Os isochron age of 102.0 ± 3.4 Ma (MSWD = 0.2). Pyrite separated from quartz–pyrite–galena–sphalerite veins (Py3) yield a Re–Os isochron age of 100.9 ± 3.1 Ma (MSWD = 0.019). Re–Os isotopic analyses of the three types of auriferous pyrite suggest that gold mineralization in the Jinchang Deposit occurred at 105.6–97.8 Ma (includes uncertainty). The initial 187Os/188Os values of the pyrites range between 0.04 and 0.60, suggesting that Os in the pyrite crystals was derived from both crust and mantle sources. |
| Author | Cai, Wen-Yan Li, Shun-Da Li, Jie Wang, Zhi-Gao Wang, Ke-Yong Peng, Da-Wei Xiao, Li |
| Author_xml | – sequence: 1 givenname: Shun-Da surname: Li fullname: Li, Shun-Da – sequence: 2 givenname: Zhi-Gao surname: Wang fullname: Wang, Zhi-Gao – sequence: 3 givenname: Ke-Yong surname: Wang fullname: Wang, Ke-Yong – sequence: 4 givenname: Wen-Yan surname: Cai fullname: Cai, Wen-Yan – sequence: 5 givenname: Da-Wei surname: Peng fullname: Peng, Da-Wei – sequence: 6 givenname: Li surname: Xiao fullname: Xiao, Li – sequence: 7 givenname: Jie surname: Li fullname: Li, Jie |
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| CitedBy_id | crossref_primary_10_1016_j_oregeorev_2023_105524 crossref_primary_10_1134_S1819714021040035 crossref_primary_10_3390_min11050480 crossref_primary_10_3390_min12060708 crossref_primary_10_1016_j_oregeorev_2019_03_018 crossref_primary_10_1016_j_oregeorev_2022_105183 crossref_primary_10_1088_1755_1315_906_1_012011 crossref_primary_10_1134_S1819714023060052 crossref_primary_10_3390_min9020099 crossref_primary_10_1002_bio_4424 crossref_primary_10_1134_S1819714021030039 |
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| Snippet | The Jinchang gold deposit is located in the eastern Yanji–Dongning Metallogenic Belt in Northeast China. The orebodies of the deposit are hosted within... |
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| SubjectTerms | Age Arsenopyrite Breccia Cement Chalcopyrite Crystals Diorite Fault lines Galena Gasoline Geochemistry Geochronology Geological time Geology Gold Gold mines & mining Magma Metallogenesis Mineralization Minerals Ores Osmium isotopes Pyrite Quartz Radiometric dating Sphalerite Veins (geology) Zincblende |
| Title | Re–Os Pyrite Geochronological Evidence of Three Mineralization Styles within the Jinchang Gold Deposit, Yanji–Dongning Metallogenic Belt, Northeast China |
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