Polymetallic Metallogenic System
Within the last decade, the high and continuing demand for precious and base metals, as well as critical elements, has prompted a global rush on a scale never before seen. This eventually resulted in the demand for considerable innovation and improvement in mineral deposit genetic modelling and ore...
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| Year of Publication: | 2019 |
| Language: | English |
| Physical Description: | 1 electronic resource (538 p.) |
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| 100 | 1 | |a Yang, Liqiang |4 auth | |
| 245 | 1 | 0 | |a Polymetallic Metallogenic System |
| 260 | |b MDPI - Multidisciplinary Digital Publishing Institute |c 2019 | ||
| 300 | |a 1 electronic resource (538 p.) | ||
| 336 | |a text |b txt |2 rdacontent | ||
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| 520 | |a Within the last decade, the high and continuing demand for precious and base metals, as well as critical elements, has prompted a global rush on a scale never before seen. This eventually resulted in the demand for considerable innovation and improvement in mineral deposit genetic modelling and ore formation regimes for the many different types of gold deposits, now recognized, and paralleled by the wide employment of exploration techniques and a rapid expansion of geological databases. This Special Issue will show case studies of porphyry polymetal systems, orogenic gold formations, water–rock reaction, ore-forming structure evolution, mineralogy and petrology of ore deposit, ore formation regime, geochronology and geochemistry of ore deposit, ore-forming evolution, mineral exploration and cutting-edge technology in ore deposit study. | ||
| 546 | |a English | ||
| 653 | |a syenite | ||
| 653 | |a petrogenesis | ||
| 653 | |a North China Craton | ||
| 653 | |a Hongyan deposit | ||
| 653 | |a Yangshan gold belt | ||
| 653 | |a mineral geo-thermometry | ||
| 653 | |a water-rock interaction | ||
| 653 | |a Pinglidian gold deposit | ||
| 653 | |a lithospheric architecture | ||
| 653 | |a Liaodong Peninsula | ||
| 653 | |a visible gold | ||
| 653 | |a Zhengchong gold deposit | ||
| 653 | |a stable isotopes | ||
| 653 | |a geochemistry | ||
| 653 | |a ore shoots | ||
| 653 | |a high fugacity | ||
| 653 | |a Huangshaping | ||
| 653 | |a zircon U-Pb dating | ||
| 653 | |a orogenic gold deposit | ||
| 653 | |a high-silica adakitic rocks (HSA) | ||
| 653 | |a zircon U-Pb dating | ||
| 653 | |a zircon geochronology | ||
| 653 | |a middle-late Jurassic | ||
| 653 | |a Rare-Earth Elements | ||
| 653 | |a Tiantangshan tin polymetallic deposit | ||
| 653 | |a whole-rock geochemistry | ||
| 653 | |a fluid inclusions | ||
| 653 | |a low Sr and high Yb A2-type granite | ||
| 653 | |a W-Sn skarn | ||
| 653 | |a Jiaodong area | ||
| 653 | |a hydrous melts | ||
| 653 | |a quartz vein | ||
| 653 | |a hydrothermal alteration halo | ||
| 653 | |a fluid inclusion | ||
| 653 | |a archean basement | ||
| 653 | |a H-O isotope | ||
| 653 | |a Sizhuang gold deposit | ||
| 653 | |a South China | ||
| 653 | |a invisible gold | ||
| 653 | |a granite petrogenesis | ||
| 653 | |a Zaorendao gold deposit | ||
| 653 | |a geostatistics | ||
| 653 | |a SE China | ||
| 653 | |a physicochemical condition of mineralization | ||
| 653 | |a metallogenesis | ||
| 653 | |a structural control | ||
| 653 | |a constraints on mineralization | ||
| 653 | |a Northwestern Yunnan Province | ||
| 653 | |a ore-forming processes | ||
| 653 | |a zircon Hf isotopes | ||
| 653 | |a metallogenic rule | ||
| 653 | |a rock geochemistry | ||
| 653 | |a Shizhuyuan | ||
| 653 | |a Sr-Nd-Pb-Hf isotopes | ||
| 653 | |a immiscibility | ||
| 653 | |a Jiaodong Peninsula | ||
| 653 | |a Mo-polymetallic deposit | ||
| 653 | |a Permian A-type granite | ||
| 653 | |a precipitation mechanism | ||
| 653 | |a Jiangnan orogenic belt | ||
| 653 | |a Chishan alkaline complex | ||
| 653 | |a A-type granite | ||
| 653 | |a in situ study | ||
| 653 | |a magmatic oxygen fugacity | ||
| 653 | |a Jiaodong | ||
| 653 | |a Liaoning Province | ||
| 653 | |a oxidation state | ||
| 653 | |a Re-Os dating | ||
| 653 | |a Saima deposit | ||
| 653 | |a C-H-O isotopes | ||
| 653 | |a sericite | ||
| 653 | |a gold deposition | ||
| 653 | |a post-collisional slab break-off | ||
| 653 | |a Hf-Nd isotopic mapping | ||
| 653 | |a geochronology | ||
| 653 | |a Sr-Nd isotopes | ||
| 653 | |a Inner Mongolia | ||
| 653 | |a Zaozigou deposit | ||
| 653 | |a Pulang porphyry Cu (-Mo-Au) deposit | ||
| 653 | |a Haoyaoerhudong gabbro | ||
| 653 | |a trace element | ||
| 653 | |a Cu-Au hydrothermal mineralization | ||
| 653 | |a molybdenite Re-Os dating | ||
| 653 | |a Hegenshan-Heihe suture zone | ||
| 653 | |a Late Cretaceous | ||
| 653 | |a Great Xing'an Range | ||
| 653 | |a SW China | ||
| 653 | |a Hongshan skarn deposit | ||
| 653 | |a tin mineralization | ||
| 653 | |a Xianghualing | ||
| 653 | |a Hf isotopes | ||
| 653 | |a post-collisional | ||
| 653 | |a hydrothermal calcite | ||
| 653 | |a molybdenite Re-Os dating | ||
| 653 | |a LA-ICP-MS zircon U-Pb dating | ||
| 653 | |a Sanshandao gold deposit | ||
| 653 | |a China | ||
| 653 | |a Lu-Hf isotopes | ||
| 653 | |a orogenic-gold deposit | ||
| 653 | |a garnet Sm-Nd dating | ||
| 653 | |a paleo-Tethyan ocean closure | ||
| 653 | |a Weilasituo Sn-polymetallic deposit | ||
| 653 | |a West Qinling | ||
| 653 | |a mantle branch | ||
| 653 | |a formation temperature | ||
| 653 | |a ore prospecting target | ||
| 653 | |a Dongbulage | ||
| 653 | |a niobium mineralization | ||
| 653 | |a LA-ICP-MS | ||
| 653 | |a quartz | ||
| 653 | |a C-O isotopes | ||
| 653 | |a acidity | ||
| 653 | |a Beiya Au deposit | ||
| 653 | |a ore-controlling structures | ||
| 653 | |a U-Pb zircon age | ||
| 653 | |a Koka deposit | ||
| 653 | |a zircon U-Pb geochronology | ||
| 653 | |a skarn mineralogy | ||
| 653 | |a Phapon gold deposit | ||
| 776 | |z 3-03921-293-1 | ||
| 906 | |a BOOK | ||
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