Polymetallic Metallogenic System
Yang, Liqiang
Polymetallic Metallogenic System
English[eng]
n/a||syenite||petrogenesis||North China Craton||Hongyan deposit||Yangshan gold belt||mineral geo-thermometry||water–rock interaction||Pinglidian gold deposit||lithospheric architecture||Liaodong Peninsula||visible gold||Zhengchong gold deposit||stable isotopes||geochemistry||ore shoots||high fugacity||Huangshaping||zircon U-Pb dating||orogenic gold deposit||high-silica adakitic rocks (HSA)||zircon U–Pb dating||zircon geochronology||middle–late Jurassic||Rare-Earth Elements||Tiantangshan tin polymetallic deposit||whole-rock geochemistry||fluid inclusions||low Sr and high Yb A2-type granite||W–Sn skarn||Jiaodong area||hydrous melts||quartz vein||hydrothermal alteration halo||fluid inclusion||archean basement||H–O isotope||Sizhuang gold deposit||South China||invisible gold||granite petrogenesis||Zaorendao gold deposit||geostatistics||SE China||physicochemical condition of mineralization||metallogenesis||structural control||constraints on mineralization||Northwestern Yunnan Province||ore-forming processes||zircon Hf isotopes||metallogenic rule||rock geochemistry||Shizhuyuan||Sr–Nd–Pb–Hf isotopes||immiscibility||Jiaodong Peninsula||Mo-polymetallic deposit||Permian A-type granite||precipitation mechanism||Jiangnan orogenic belt||Chishan alkaline complex||A-type granite||in situ study||magmatic oxygen fugacity||Jiaodong||Liaoning Province||oxidation state||Re–Os dating||Saima deposit||C–H–O isotopes||sericite||gold deposition||post-collisional slab break-off||Hf-Nd isotopic mapping||geochronology||Sr–Nd isotopes||Inner Mongolia||Zaozigou deposit||Pulang porphyry Cu (–Mo–Au) deposit||Haoyaoerhudong gabbro||trace element||Cu-Au hydrothermal mineralization||molybdenite Re-Os dating||Hegenshan-Heihe suture zone||Late Cretaceous||Great Xing’an Range||SW China||Hongshan skarn deposit||tin mineralization||Xianghualing||Hf isotopes||post-collisional||hydrothermal calcite||molybdenite Re–Os dating||LA-ICP-MS zircon U–Pb dating||Sanshandao gold deposit||China||Lu–Hf isotopes||orogenic-gold deposit||garnet Sm–Nd dating||paleo-Tethyan ocean closure||Weilasituo Sn-polymetallic deposit||West Qinling||mantle branch||formation temperature||ore prospecting target||Dongbulage||niobium mineralization||LA-ICP-MS||quartz||C–O isotopes||acidity||Beiya Au deposit||ore-controlling structures||U–Pb zircon age||Koka deposit||zircon U–Pb geochronology||skarn mineralogy||Phapon gold deposit
Polymetallic Metallogenic System
English[eng]
n/a||syenite||petrogenesis||North China Craton||Hongyan deposit||Yangshan gold belt||mineral geo-thermometry||water–rock interaction||Pinglidian gold deposit||lithospheric architecture||Liaodong Peninsula||visible gold||Zhengchong gold deposit||stable isotopes||geochemistry||ore shoots||high fugacity||Huangshaping||zircon U-Pb dating||orogenic gold deposit||high-silica adakitic rocks (HSA)||zircon U–Pb dating||zircon geochronology||middle–late Jurassic||Rare-Earth Elements||Tiantangshan tin polymetallic deposit||whole-rock geochemistry||fluid inclusions||low Sr and high Yb A2-type granite||W–Sn skarn||Jiaodong area||hydrous melts||quartz vein||hydrothermal alteration halo||fluid inclusion||archean basement||H–O isotope||Sizhuang gold deposit||South China||invisible gold||granite petrogenesis||Zaorendao gold deposit||geostatistics||SE China||physicochemical condition of mineralization||metallogenesis||structural control||constraints on mineralization||Northwestern Yunnan Province||ore-forming processes||zircon Hf isotopes||metallogenic rule||rock geochemistry||Shizhuyuan||Sr–Nd–Pb–Hf isotopes||immiscibility||Jiaodong Peninsula||Mo-polymetallic deposit||Permian A-type granite||precipitation mechanism||Jiangnan orogenic belt||Chishan alkaline complex||A-type granite||in situ study||magmatic oxygen fugacity||Jiaodong||Liaoning Province||oxidation state||Re–Os dating||Saima deposit||C–H–O isotopes||sericite||gold deposition||post-collisional slab break-off||Hf-Nd isotopic mapping||geochronology||Sr–Nd isotopes||Inner Mongolia||Zaozigou deposit||Pulang porphyry Cu (–Mo–Au) deposit||Haoyaoerhudong gabbro||trace element||Cu-Au hydrothermal mineralization||molybdenite Re-Os dating||Hegenshan-Heihe suture zone||Late Cretaceous||Great Xing’an Range||SW China||Hongshan skarn deposit||tin mineralization||Xianghualing||Hf isotopes||post-collisional||hydrothermal calcite||molybdenite Re–Os dating||LA-ICP-MS zircon U–Pb dating||Sanshandao gold deposit||China||Lu–Hf isotopes||orogenic-gold deposit||garnet Sm–Nd dating||paleo-Tethyan ocean closure||Weilasituo Sn-polymetallic deposit||West Qinling||mantle branch||formation temperature||ore prospecting target||Dongbulage||niobium mineralization||LA-ICP-MS||quartz||C–O isotopes||acidity||Beiya Au deposit||ore-controlling structures||U–Pb zircon age||Koka deposit||zircon U–Pb geochronology||skarn mineralogy||Phapon gold deposit