大地構(gòu)造與成礦(島弧與活動(dòng)大陸邊緣)

1、外部隆起海溝坡折（又稱構(gòu)造隆起、構(gòu)造弧、外弧脊）弧溝間隙（包括弧前盆地）巖漿?。ㄓ址Q內(nèi)弧、主弧、火山弧）活動(dòng)邊緣海盆地（又稱弧間盆地）殘余?。ㄓ址Q死弧、第三?。┖弦粛u弧構(gòu)造地形單元?jiǎng)澐趾弦粛u弧構(gòu)造地形單元?jiǎng)澐只『笈璧谽ast facing continental margin亞州東部日本海東亞大陸West facing continent巴西和智利外部隆起海溝坡折（又稱構(gòu)造隆起、構(gòu)造弧、外弧脊）巖漿?。ㄓ址Q內(nèi)弧、主弧、火山?。﹏弧間盆地2）Mineral Deposits in outer arc早期早期中期中期晚期晚期3）Mineral deposits of Outer arc tro

2、ugh早期早期Interpretative geological sections through Nias and Sumatran continental Margin showing Neogene evolution早中新世presentYoung this sideFigure showing the formation process of anOuter arcIdeal model showing sediments subductionAnd subduction erosion沉積物俯沖底侵作用4）Mineral deposits of magmatic arcs4）Min

3、eral deposits of magmatic arcsKuroko depositBesshi deposits5）Deposit types in back-arc thrust beltWest facing continentinactiveactiveSchematic cross-section through the Andes near northern end of Bolivian tin beltTinSchematic cross-section through the Andes 早期階段早期階段晚期階段晚期階段Postmagmatic stageEarly Hy

4、drothermalLate HydrothermalThermal springspropyliticLevel of Cu deposit After erosionDiorite-related porphyry modelSchematic representation of the sequential filling stages ofthe gold-bearing, quartzsulfide veins at the Ge ant Dormantdeposit.Dialation zones含子礦物不含子礦物4、礦床成因1）成礦溫度）成礦溫度2）熱液成分）熱液成分始熔溫度熔化

5、溫度均一溫度部分均一溫度Fault valve stagesPlume subductionGenetical model for generating lithosphere-scale thermal anomalies and to drive orogen-scale hydrothermal systemsCrustal thickingOceanic ridge subductionSubduction rollbackErosion of mantle lithosphereDeclamation of mantle lithosphere（3）成礦時(shí)代）成礦時(shí)代Ore is commonly deposited as open