06110nam 22018013a 450 991036775930332120250203235426.09783039212941303921294X10.3390/books978-3-03921-294-1(CKB)4100000010106124(oapen)https://directory.doabooks.org/handle/20.500.12854/56643(ScCtBLL)e2dd0a58-3638-49b6-b649-b6349d7f74c0(OCoLC)1163849929(EXLCZ)99410000001010612420250203i20192019 uu engurmn|---annantxtrdacontentcrdamediacrrdacarrierPolymetallic Metallogenic SystemLiqiang YangBasel, Switzerland :MDPI,2019.1 electronic resource (538 p.)9783039212934 3039212931 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.syenitepetrogenesisNorth China CratonHongyan depositYangshan gold beltmineral geo-thermometrywater-rock interactionPinglidian gold depositlithospheric architectureLiaodong Peninsulavisible goldZhengchong gold depositstable isotopesgeochemistryore shootshigh fugacityHuangshapingzircon U-Pb datingorogenic gold deposithigh-silica adakitic rocks (HSA)zircon U-Pb datingzircon geochronologymiddle-late JurassicRare-Earth ElementsTiantangshan tin polymetallic depositwhole-rock geochemistryfluid inclusionslow Sr and high Yb A2-type graniteW-Sn skarnJiaodong areahydrous meltsquartz veinhydrothermal alteration halofluid inclusionarchean basementH-O isotopeSizhuang gold depositSouth Chinainvisible goldgranite petrogenesisZaorendao gold depositgeostatisticsSE Chinaphysicochemical condition of mineralizationmetallogenesisstructural controlconstraints on mineralizationNorthwestern Yunnan Provinceore-forming processeszircon Hf isotopesmetallogenic rulerock geochemistryShizhuyuanSr-Nd-Pb-Hf isotopesimmiscibilityJiaodong PeninsulaMo-polymetallic depositPermian A-type graniteprecipitation mechanismJiangnan orogenic beltChishan alkaline complexA-type granitein situ studymagmatic oxygen fugacityJiaodongLiaoning Provinceoxidation stateRe-Os datingSaima depositC-H-O isotopessericitegold depositionpost-collisional slab break-offHf-Nd isotopic mappinggeochronologySr-Nd isotopesInner MongoliaZaozigou depositPulang porphyry Cu (-Mo-Au) depositHaoyaoerhudong gabbrotrace elementCu-Au hydrothermal mineralizationmolybdenite Re-Os datingHegenshan-Heihe suture zoneLate CretaceousGreat Xing'an RangeSW ChinaHongshan skarn deposittin mineralizationXianghualingHf isotopespost-collisionalhydrothermal calcitemolybdenite Re-Os datingLA-ICP-MS zircon U-Pb datingSanshandao gold depositChinaLu-Hf isotopesorogenic-gold depositgarnet Sm-Nd datingpaleo-Tethyan ocean closureWeilasituo Sn-polymetallic depositWest Qinlingmantle branchformation temperatureore prospecting targetDongbulageniobium mineralizationLA-ICP-MSquartzC-O isotopesacidityBeiya Au depositore-controlling structuresU-Pb zircon ageKoka depositzircon U-Pb geochronologyskarn mineralogyPhapon gold depositYang Liqiang1317917ScCtBLLScCtBLLBOOK9910367759303321Polymetallic Metallogenic System3033090UNINA