图  1  汤丹铜矿床（SSC型）4号构造岩相学实测纵剖面

1—震旦系陡山沱组；2—中元古界东川群落雪组二段；3—中元古界东川群落雪组一段； 4—中元古界东川群因民组三段；5—古元古界汤丹岩群平顶山组；6—铁质板岩；7—白云岩； 8—泥粉砂质板岩；9—碱性铁质辉绿辉长岩枝（墙）；10—铜矿体（SSC型铜矿床）；11—低品位铜矿体； 12—推测铜矿体；13—地质界线； 14—推测地质界线；15—断层；16—推测断层； 17—地质产状；18—中段标高和海拔高度

Figure  1.  Measured No.4 longitudinal profiles of tectonic lithofacies in the Tangdan copper deposits (SSC-type)

1−Sinian Doushantuo Formation; 2−the Second of member at Luoxue Formation of Mesoproterozoic Dongchuan Group; 3−the first member at Luoxue Formation of Mesoproterozoic Dongchuan Group; 4−the three member at Yinming Formation of Mesoproterozoic Dongchuan Group; 5−Pingdingshan Formation of Palaeoproterozoic Tangdan Rock Group; 6−irony slate; 7−dolomite; 8−argillaceous-silty slate; 9−alkaline Fe-rich diabase-gabbro apophyse or dike; 10−copper orebody（SSC-type copper deposit）；11−copper orebody with low-grades; 12−presumed copper orebody；13−geological line; 14−presumable geological line；15−faults; 16−presumed faults; 17−geological occurrence; 18−adit level and above the sea level

图  2  白锡腊−中老龙IOCG型和SSC型铜矿床实测构造岩相学纵剖面

1—中元古界东川群落雪组二段；2—中元古界东川群落雪组一段；3—中元古界东川群因民组三段；4—碱性铁质辉绿辉长岩枝；5—热液角砾岩相；6—铜矿体（SSC型铜矿床）；7—低品位铜矿体；8—铁铜矿体（IOCG型铁铜矿床）；9—地质界线；10. —推测地质界线；11—断层；12—穿脉垂直投影面；13—坑内钻孔及编号；14—中段标高和海拔高度；15—地质产状

Figure  2.  Measured longitudinal profiles of tectonic lithofacies for IOCG-type and SSC-type copper deposits from Baixila to Zhonglaolong

1−the second of member of the Luoxue Formation of the Mesoproterozoic Dongchuan Group; 2−the first member of the Luoxue Formation of the Mesoproterozoic Dongchuan Group; 3−the third member of the Yinming Formation of the Mesoproterozoic Dongchuan Group; 4−alkaline Fe-rich diabase-gabbro apophyse; 5−hydrothermal breccia facies; 6−copper orebody (SSC-type copper deposit); 7−low-grade copper orebody; 8−Fe-Cu orebody (IOCG-type deposit); 9−geological boundary; 10−inferred geological boundary; 11−fault; 12−transverse drift (vertical projection); 13−adit-in drillhole and its number; 14−adit elevation and altitude

图  3  甲查银多金属矿田火山机构与矿田构造岩相图

a—甲乌拉−查干银多金属矿田构造岩相图；b—e、h—j为甲乌拉银多金属矿床；f—g为查干银多金属矿床；b—540 m中段铅锌硫化物充填交代脉与边部菱沸石−铁绿泥石相；c—580 m中段石膏−蒙脱石−钾伊利石相；d—580 m中段伊蒙混层−伊利石相；e—475 m中段细脉状和微脉状闪锌矿方铅矿硫化物充填在伊利石热液角砾岩相中。 f—怡圣园西端18号矿体300 m中段216勘探线主巷道掌子面富银菱锰矿铁锰碳酸盐热液角砾岩相；g—怡圣园西端18号矿体300 m中段216勘探线主巷道掌子面富银菱锰矿铁锰碳酸盐热液角砾岩相；h—200 m中段5′—7′线含闪锌矿方铅矿马牙状石英脉；i—伟晶状方铅矿结晶核相；j—200 m中段5′—7′线2号矿体巨晶状方铅矿结晶核相的外缘中心相（具有海绵陨铁结构的铁闪锌矿−磁黄铁矿−黄铜矿矿石，磁化率151～114×10⁻³SI）

Figure  3.  Mapping of volcanic edifice and ore-field tectonic lithofacies in the Jia–Cha Ag-polymetallic orefield

(a) Tectonic lithofacies map of the Jiawula–Chagan Ag-polymetallic orefield; Fig.3b to 3e and 3h to 3i are photos from the Jiawula Ag-polymetallic deposit and Fig.3f to 3g are photos from the Chagan Ag-polymetallic deposit; (b) Chabasite-daphnite facies along both sides of the filling−replacement veins of Pb-Zn-sulfides at 540 m level; (c) Gypsum-semctite-K-illite facies at 580 m level; (d) Facies of illite-smectite formation and illite at 580 m level; (e) Fine-veined and microveined sphalerite-galena sulfides veins filling in lithofacies of illite hydrothermal breccia at 475 m level; (f) Fe-Mn-carbonate hydrothermal breccia lithofacies of Ag-rich rhodochrosite from No.18 orebody in the 216 exploration line at the tunnel face of 300 m level; (g) Fe-Mn-carbonate hydrothermal breccia lithofacies of Ag-rich rhodochrosite from No.18 orebody in the 216 exploration line at the tunnel face of 300 m level; (h) Sphalerite-galena sulfides quartz veins in horse-teeth-shape in the 5′–7′ exploration line at 200 m level; (i) Crystalline nuclear lithofacies of pegmatitic galena in the 5′–7′ exploration line at 200 m level; (j) Marmatite-pyrrhotite-chalcopyrite ores in sideronitic texture around crystalline nuclear lithofacies of pegmatitic galena in the 5′–7′ exploration line at 200 m level; magnetic susceptibility is from 151×10⁻³ to 114×10⁻³SI

图  4  个旧老厂矿田电气石热流柱构造与实测构造岩相学剖面图

Figure  4.  Measured profiles of tectonic lithofacies of tourmaline plume tectonics in the Laochang orefield, Gejiu