Zircon U–Pb and molybdenite Re–Os geochronology and geochemistry of Jinchang porphyry gold–copper deposit, NE China: Two-phase mineralization and the tectonic setting

[Display omitted] •The Jinchang gold-rich porphyry deposit has experienced two mineralization phases.•It includes early Au–Cu (∼114 Ma) and late Au-only mineralization (103–101 Ma).•Jinchang deposit was formed by the subduction roll-back of the Paleo-Pacific Plate. Whether multiple mineralization st...

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Published inOre geology reviews Vol. 107; pp. 735 - 753
Main Authors Cai, Wen-yan, Wang, Zhi-gao, Li, Jian, Fu, Li-juan, Wang, Ke-yong, Konare, Yassa, Li, Shun-da
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.04.2019
Subjects
Central Asian Orogenic Belt
Molybdenite Re–Os dating
NE China
Paleo-Pacific plate
Porphyry deposits
Zircon U–Pb dating
Molybdenite Re–Os dating
Central Asian Orogenic Belt
Paleo-Pacific plate
Porphyry deposits
NE China
Zircon U–Pb dating
Online AccessGet full text
ISSN0169-1368
1872-7360
DOI10.1016/j.oregeorev.2019.03.018

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Abstract [Display omitted] •The Jinchang gold-rich porphyry deposit has experienced two mineralization phases.•It includes early Au–Cu (∼114 Ma) and late Au-only mineralization (103–101 Ma).•Jinchang deposit was formed by the subduction roll-back of the Paleo-Pacific Plate. Whether multiple mineralization styles in porphyry deposits are the result of one or multiple pulses of magmatism is unknown. In this paper, we present new age and geochemical data on the Jinchang porphyry gold-copper (Au-Cu) deposit, an important deposit in NE China and in the eastern Central Asian Orogenic Belt (CAOB). Field geological study suggests that both the mineralization and ore-causative magmatism at Jinchang are multiphase. LA-ICP-MS zircon U-Pb dating of the monzogranite ore host yielded 197 ± 1 Ma, which is considerably older than the ore-causative monzonite (115 ± 3 Ma) and granodiorite (107 ± 2 Ma). Molybdenite Re–Os dating on the breccia pipe-hosted Au-Cu ores yielded a well-defined isochron age of 114 ± 3 Ma, coeval to the monzonite emplacement. The Au-Cu mineralization was followed by another phase of crypto-explosive breccia pipe-hosted, disseminated/vein-type Au mineralization. This Au-only mineralization phase was auriferous pyrite Re–Os dated to be 103–101 Ma, coeval to the granodiorite emplacement. Geochemically, the monzonite and granodiorite are enriched in LILEs and LREEs, but depleted in HFSEs and HREEs. The ore-causative rocks are I-type and display continental arc geochemical affinities. We suggest that the monzonite and granodiorite were generated in an intracontinental extensional setting, probably caused by the Early Cretaceous subduction roll-back of the Paleo-Pacific Plate.
AbstractList [Display omitted] •The Jinchang gold-rich porphyry deposit has experienced two mineralization phases.•It includes early Au–Cu (∼114 Ma) and late Au-only mineralization (103–101 Ma).•Jinchang deposit was formed by the subduction roll-back of the Paleo-Pacific Plate. Whether multiple mineralization styles in porphyry deposits are the result of one or multiple pulses of magmatism is unknown. In this paper, we present new age and geochemical data on the Jinchang porphyry gold-copper (Au-Cu) deposit, an important deposit in NE China and in the eastern Central Asian Orogenic Belt (CAOB). Field geological study suggests that both the mineralization and ore-causative magmatism at Jinchang are multiphase. LA-ICP-MS zircon U-Pb dating of the monzogranite ore host yielded 197 ± 1 Ma, which is considerably older than the ore-causative monzonite (115 ± 3 Ma) and granodiorite (107 ± 2 Ma). Molybdenite Re–Os dating on the breccia pipe-hosted Au-Cu ores yielded a well-defined isochron age of 114 ± 3 Ma, coeval to the monzonite emplacement. The Au-Cu mineralization was followed by another phase of crypto-explosive breccia pipe-hosted, disseminated/vein-type Au mineralization. This Au-only mineralization phase was auriferous pyrite Re–Os dated to be 103–101 Ma, coeval to the granodiorite emplacement. Geochemically, the monzonite and granodiorite are enriched in LILEs and LREEs, but depleted in HFSEs and HREEs. The ore-causative rocks are I-type and display continental arc geochemical affinities. We suggest that the monzonite and granodiorite were generated in an intracontinental extensional setting, probably caused by the Early Cretaceous subduction roll-back of the Paleo-Pacific Plate.
Author Cai, Wen-yan
Fu, Li-juan
Li, Shun-da
Konare, Yassa
Wang, Zhi-gao
Wang, Ke-yong
Li, Jian
Author_xml – sequence: 1
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  fullname: Cai, Wen-yan
  organization: College of Earth Sciences, Jilin University, Changchun 130061, China
– sequence: 2
  givenname: Zhi-gao
  surname: Wang
  fullname: Wang, Zhi-gao
  organization: College of Exploration and Surveying Engineering, Changchun Institute of Technology, Changchun 130061, China
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  surname: Li
  fullname: Li, Jian
  organization: College of Earth Sciences, Jilin University, Changchun 130061, China
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  givenname: Li-juan
  surname: Fu
  fullname: Fu, Li-juan
  organization: Shandong Gold Geological Survey Co. Ltd. (Inner Mongolia), Chifeng, China
– sequence: 5
  givenname: Ke-yong
  surname: Wang
  fullname: Wang, Ke-yong
  email: wangky@jlu.edu.cn
  organization: College of Earth Sciences, Jilin University, Changchun 130061, China
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  givenname: Yassa
  surname: Konare
  fullname: Konare, Yassa
  organization: IAMGOLD Exploration Mali Sarl, Bamako 2699, Mali
– sequence: 7
  givenname: Shun-da
  surname: Li
  fullname: Li, Shun-da
  organization: College of Earth Sciences, Jilin University, Changchun 130061, China
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Keywords Molybdenite Re–Os dating
Central Asian Orogenic Belt
Paleo-Pacific plate
Porphyry deposits
NE China
Zircon U–Pb dating
Language English
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Snippet [Display omitted] •The Jinchang gold-rich porphyry deposit has experienced two mineralization phases.•It includes early Au–Cu (∼114 Ma) and late Au-only...
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StartPage 735
SubjectTerms Central Asian Orogenic Belt
Molybdenite Re–Os dating
NE China
Paleo-Pacific plate
Porphyry deposits
Zircon U–Pb dating
Title Zircon U–Pb and molybdenite Re–Os geochronology and geochemistry of Jinchang porphyry gold–copper deposit, NE China: Two-phase mineralization and the tectonic setting
URI https://dx.doi.org/10.1016/j.oregeorev.2019.03.018
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