Thermal history of the giant Qulong Cu–Mo deposit, Gangdese metallogenic belt, Tibet: Constraints on magmatic–hydrothermal evolution and exhumation

A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented. Zircon U–Pb geochronology indicates that the mineralization at Qulong resulted from brecciation-veining events associated with the emplacement of a series of intermediate-felsic intrusions. Combined with previously...

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Published inGondwana research Vol. 36; pp. 390 - 409
Main Authors Zhao, Junxing, Qin, Kezhang, Xiao, Bo, McInnes, Brent, Li, Guangming, Evans, Noreen, Cao, Mingjian, Li, Jinxiang
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.08.2016
Subjects
Cooling-exhumation process
Gangdese
Qulong Cu–Mo deposit
Thermochronology
U–Pb and Ar–Ar geochronology
Cooling-exhumation process
Qulong Cu–Mo deposit
Gangdese
Thermochronology
U–Pb and Ar–Ar geochronology
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Abstract A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented. Zircon U–Pb geochronology indicates that the mineralization at Qulong resulted from brecciation-veining events associated with the emplacement of a series of intermediate-felsic intrusions. Combined with previously published ages, our results reveal a whole intrusive history of the Qulong composite pluton. Causative porphyries were emplaced at ~16.0Ma as revealed by 40Ar–39Ar dating of hydrothermal biotite (15.7±0.2Ma) and sericite (15.7±0.2Ma). Zircon and apatite (U–Th)/He (ZHe and AHe) dating of Qulong revealed that both followed similar, monotonic thermal trajectories from 900°C (U–Pb ages: 17.5–15.9Ma) to 200°C (ZHe: 15.7–14.0Ma), and that the causative porphyries experienced faster cooling at a maximum rate of greater than 200°C/myr. The Qulong deposit was exhumed between 13.6Ma and 12.4Ma (AHe) at an estimated rate of 0.16–0.24mm/y, which is consistent with previous estimates for other Gangdese Miocene porphyry deposits. Our AHe thermochronology results suggest that neither the Gangdese thrust system, nor the Yadong–Gulu graben affected or accelerated exhumation at the Qulong deposit. [Display omitted] •The first paired ZHe and AHe thermochronological investigations at Qulong.•Hypogene processes happened during ~1Ma at a high cooling rate of over 200°C/myr.•The Qulong deposit began to be exhumed from 13.6–12.4Ma at rate of 0.16–0.24mm/y.
AbstractList A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented. Zircon U–Pb geochronology indicates that the mineralization at Qulong resulted from brecciation-veining events associated with the emplacement of a series of intermediate-felsic intrusions. Combined with previously published ages, our results reveal a whole intrusive history of the Qulong composite pluton. Causative porphyries were emplaced at ~16.0Ma as revealed by 40Ar–39Ar dating of hydrothermal biotite (15.7±0.2Ma) and sericite (15.7±0.2Ma). Zircon and apatite (U–Th)/He (ZHe and AHe) dating of Qulong revealed that both followed similar, monotonic thermal trajectories from 900°C (U–Pb ages: 17.5–15.9Ma) to 200°C (ZHe: 15.7–14.0Ma), and that the causative porphyries experienced faster cooling at a maximum rate of greater than 200°C/myr. The Qulong deposit was exhumed between 13.6Ma and 12.4Ma (AHe) at an estimated rate of 0.16–0.24mm/y, which is consistent with previous estimates for other Gangdese Miocene porphyry deposits. Our AHe thermochronology results suggest that neither the Gangdese thrust system, nor the Yadong–Gulu graben affected or accelerated exhumation at the Qulong deposit. [Display omitted] •The first paired ZHe and AHe thermochronological investigations at Qulong.•Hypogene processes happened during ~1Ma at a high cooling rate of over 200°C/myr.•The Qulong deposit began to be exhumed from 13.6–12.4Ma at rate of 0.16–0.24mm/y.
Author Zhao, Junxing
Li, Guangming
Li, Jinxiang
Qin, Kezhang
Cao, Mingjian
Evans, Noreen
Xiao, Bo
McInnes, Brent
Author_xml – sequence: 1
  givenname: Junxing
  surname: Zhao
  fullname: Zhao, Junxing
  email: junxingzhao@gmail.com
  organization: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beitucheng West Road 19#, Chaoyang District, Beijing 100029, China
– sequence: 2
  givenname: Kezhang
  surname: Qin
  fullname: Qin, Kezhang
  email: kzq@mail.iggcas.ac.cn
  organization: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beitucheng West Road 19#, Chaoyang District, Beijing 100029, China
– sequence: 3
  givenname: Bo
  surname: Xiao
  fullname: Xiao, Bo
  organization: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beitucheng West Road 19#, Chaoyang District, Beijing 100029, China
– sequence: 4
  givenname: Brent
  surname: McInnes
  fullname: McInnes, Brent
  organization: John de Laeter Center for Isotope Research, TIGeR, Department of Applied Geology/Applied Physics, Curtin University, Perth, WA6945, Australia
– sequence: 5
  givenname: Guangming
  surname: Li
  fullname: Li, Guangming
  organization: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beitucheng West Road 19#, Chaoyang District, Beijing 100029, China
– sequence: 6
  givenname: Noreen
  surname: Evans
  fullname: Evans, Noreen
  organization: John de Laeter Center for Isotope Research, TIGeR, Department of Applied Geology/Applied Physics, Curtin University, Perth, WA6945, Australia
– sequence: 7
  givenname: Mingjian
  surname: Cao
  fullname: Cao, Mingjian
  organization: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beitucheng West Road 19#, Chaoyang District, Beijing 100029, China
– sequence: 8
  givenname: Jinxiang
  surname: Li
  fullname: Li, Jinxiang
  organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Qinghai-Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Road, Chaoyang District, Beijing 100085, China
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Keywords Cooling-exhumation process
Qulong Cu–Mo deposit
Gangdese
Thermochronology
U–Pb and Ar–Ar geochronology
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Snippet A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented. Zircon U–Pb geochronology indicates that the mineralization at Qulong...
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elsevier
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Index Database
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StartPage 390
SubjectTerms Cooling-exhumation process
Gangdese
Qulong Cu–Mo deposit
Thermochronology
U–Pb and Ar–Ar geochronology
Title Thermal history of the giant Qulong Cu–Mo deposit, Gangdese metallogenic belt, Tibet: Constraints on magmatic–hydrothermal evolution and exhumation
URI https://dx.doi.org/10.1016/j.gr.2015.07.005
Volume 36
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