Geochronological and geochemical constraints on the ore-related granites in Huanggang deposit, Southern Great Xing’an Range, NE China and its tectonic significance
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  • 作者:Wei Mei ; Xinbiao ; Zhi Liu ; Rankun Tang ; Zhilong Ai…
  • 关键词:Huanggang ; ore ; related granite ; U ; Pb dating ; geochemistry ; Southern Great Xing’an Range
  • 刊名:Geosciences Journal
  • 出版年:2015
  • 出版时间:March 2015
  • 年:2015
  • 卷:19
  • 期:1
  • 页码:53-67
  • 全文大小:1,199 KB
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  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geosciences
  • 出版者:The Geological Society of Korea, co-published with Springer
  • ISSN:1598-7477
文摘
Huanggang skarn Fe-Sn deposit is located in the main ridge Sn-polymetallic metallogenic sub-belt of the Southern Great Xing’an Range. A combination of zircon U-Pb age, geochemistry and Hf isotopic composition are reported for the orerelated granite (K-feldspar granite) of the Huanggang deposit to constrain its petrogenesis and tectonic setting. LA-ICP-MS U-Pb Zircon dating results indicate that the K-feldspar granite was intruded at 145.3 ± 1.6Ma. The K-feldspar granites belong to high-K calc-alkaline and shoshonite series, mainly peraluminous. These rocks have a negative slope from La to Lu with strongly negative Eu anomalies, they demonstrate negative Ba, Sr P, Ti and Nb spikes and positive Th, U, Nd spikes on the normalized incompatible element diagrams. The regional geological setting together with the geochemistry of the K-feldspar granite indicates that it is formed in a post-orogenic setting. The zircon Hf isotopic compositions (?Hf(t): +5.2 to +6.6, 176Hf/177Hf: 0.282837-.282876) indicate both juvenile crust sources that originated from depleted mantle and some ancient continental crust sources contributed to its origin, and there is a significant addition of juvenile crust under the Southern Great Xing’an Range during the time from Paleo-Neoproterozoic to Phanerozoic.

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