Geophysical field characteristics and deep ore prospecting prediction of the Nannihu molybdenum lead-zinc-silver polymetallic ore field in East Qinling Mountain
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摘要:
南泥湖钼多金属矿田是中国重要的钼（钨）铅锌银多金属矿产地，已探明超大型钼（钨）矿床3处，大型钼（钨）矿床3处，中、大型铅锌银（金）矿床10余处。矿田具有优越的地质成矿条件，深部找矿潜力巨大。现有矿产勘查深度主要是500 m以浅范围，深部（500～2000 m）找矿工作基本为空白，需要使用综合地球物理方法研究深部成矿规律，预测新的矿产资源。文章通过研究该区地质、地球物理场特征和典型矿床物探异常特征，取得了有意义的研究成果。（1）确定了与成矿关系密切的隐伏岩体侵入模型：将全区隐伏岩体从南至北分为3个区，Ⅰ区隐伏岩体顶面深度0～800 m，分布面积约125 km2；Ⅱ区隐伏岩体顶面深度0.8～1.5 km，分布面积约158 km2；Ⅲ区隐伏岩体顶面深度1.5～3 km，分布面积约233 km2。（2）建立了立体成矿模型（根据成矿空间位置的不同从地表向下分为4个空间成矿区）和综合地球物理找矿模型（包括隐伏岩体、隐伏岩体顶上带、岩钟和斑岩体、矿体和矿化体的地球物理场标志）。（3）指出隐伏岩体顶上带及其上方的岩钟、岩脉、岩枝和小斑岩体等是成矿有利部位。（4）预测了找矿潜力；总结了寻找钼钨铅锌银金矿产的勘查方法技术组合。研究成果对在该区和类似矿区进行深部找矿工作具有重要意义。
Abstract:The Nannihu molybdenum polymetallic orefield is an important production area of Mo (W) Pb, Zn, Ag polymetallic ore resources in China, which includes 3 proven super large molybdenum (tungsten) deposit, 3 large molybdenum (tungsten) deposits, and more than 10 medium and large Pb Zn Ag (Au) deposits. The orefield has superior geological metallogenic conditions and deep prospecting potential. The depth of the existing mineral exploration is mainly 500m to a shallow range, and the deep (500-2000 m) prospecting work is basically blank. It is necessary to use the integrated geophysical method to study the metallogenic regularity and predict the new mineral resources. By studying the geological and geophysical characteristics of the area and the geophysical anomalies of the typical deposits, significant research results have been obtained:(1) The intrusion model of the concealed rock mass is established, which is closely related to the mineralization. The whole concealed rocks are divided into three zones from south to north; the depth of the top of the buried rock is 0～800 m, and the distribution area is about 125 km2; the depth of the top of the buried rock is 0.8-1.5 km, and its distribution area is about 158 km2; the depth of the top surface of the buried rock is 1.5-3 km, and its distribution area is about 233 km2. (2) The three-dimensional metallogenic model, which is divided into four spatial metallogenic regions from the surface according to the different spatial locations of mineralization, and integrated geophysical prospecting model (the geophysical field marks of the concealed rock mass, the upper zone of the concealed rock mass, the kupola and the porphyry, the ore bodies and the mineralized bodies) are established. (3) It is pointed out that the concealed rock top belt and the kupola above it, dikes, apophyse and porphyry are favorable sites of mineralization. (4) Ore prospecting potential is predicted; the methods for prospecting of tungsten and molybdenum lead-zinc-silver gold mineral deposits are summarized. The research results have important significance for deep prospecting in this area and similar mining areas.
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图 1 南泥湖矿集区矿产地质略图（据段士刚等，2011修改）
1—新生界古近-新近系；2—下古生界陶湾群；3—新元古界栾川群；4—中元古界官道口群；5—中元古界熊耳群；6—太古宇太华群；7—燕山期小斑岩侵入体；8—新元古界正长斑岩；9—新元古界辉长岩；10—中元古界碱性花岗岩；11—断层；12—逆冲断层；13—正断层；14—地质界线；15—不整合接触；16—超大型钼(钨)矿床；17—大型钼(钨)矿床；18—中型钼矿床；19—铅锌银矿床；20—金（银铅）矿床；21—多金属硫铁矿床
Figure 1. Geological sketch map of the Nannihu ore concentration area (modified after Duan Shigang et al., 2011)
1- Cenozoic Paleogene-Neogene; 2- Lower Paleozoic Taowan Group; 3- Neoproterozoic Luanchuan Group; 4- middle Proterozoic Guandaokou Group; 5- middle Proterozoic Xiong'er Group; 6- Archean Taihua Group; 7- Yanshanian small porphyry intrusive body; 8- Neoproterozoic syenite porphyry; 9- Neoproterozoic gabbro; 10- Mesoproterozoic alkaline granite; 11- Fault; 12- Thrust fault; 13- Normal fault; 14- Geological boundary; 15- Unconformity contact; 16- Superlarge molybdenum (tungsten) ore deposit; 17- Large molybdenum (tungsten) ore deposit; 18- Medium sized molybdenum deposit; 19-Lead-zinc silver deposit; 20-Gold (silver lead) deposit; 21- Polymetallic sulfur iron ore deposit
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图 2 南泥湖矿集区重磁异常图
1—重力等值线；2—航磁△T正等值线；3—航磁△T负等值线；4—航磁△T零等值线；5—推断隐伏岩体范围；6—超大型钼(钨)矿床；7—大型钼(钨)矿床；8—中型钼矿床；9—铅锌银矿床；10—金（银铅）矿床；11—多金属硫铁矿床
Figure 2. Gravity and magnetic anomaly map of the Nannihu ore concentration area
1-Gravity contour; 2-△T positive aeromagnetic isoline; 3-△T negative aeromagnetic isoline; 4-△T aeromagnetic zero isoline; 5-Inferred concealed rock; 6-Superlarge molybdenum (tungsten) ore deposit; 7-Large molybdenum (tungsten) ore deposit; 8-Medium molybdenum deposit; 9-Lead-zinc-silver deposit; 10-gold (silver-lead) deposit; 11-Polymetallic sulfur iron ore deposit
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图 3 南泥湖矿集区重力异常反演拟合剖面图（据王纪中等，2010修改）
1—中、新元古界官道口群、栾川群；2—中元古界熊耳群；3—太古宇太华群；4—燕山期酸性岩体；5—重力原始、拟合异常
Figure 3. Fitting section of gravity anomaly inversion in the Nannihu ore concentration area (modified from Wang Jizhong et al., 2010)
1 - Middle Proterozoic and Neoproterozoic Guandaokou Group, Luanchuan Group; 2- Mesoproterozoic Xiong'er Group; 3- Archean Taihua Group; 4- Acidic rock mass in Yanshanian period; 5-Gravity primitive and fitting anomaly
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图 4 罗村钼矿区04勘探线地质物探综合剖面图
1—花岗斑岩；2—花岗角砾岩；3—花岗闪长岩；4—花岗闪长角砾岩；5—中粗粒花岗岩；6—辉绿岩；7—工业品位矿体；8—边界品位矿体；9—推断钼矿体
Figure 4. Comprehensive section of geological and geophysical of the 04 exploration line in the Luocun molybdenum mine area
1-Granite porphyry; 2-Granite breccia; 3-Granodiorite; 4-Granodiorite breccia; 5-Medium coarse grained granite; 6-diabase; 7-Industrial grade ore body; 8-Boundary grade ore body; 9-Inferring molybdenum ore body
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图 5 南泥湖矿集区重磁推断隐伏岩体图
1—深度0～800 m隐伏岩体范围；2—深度0.8～1.5 km隐伏岩体范围；3—深度1.5～3 km隐伏岩体范围；4—围岩地层（从北至南为中元古界熊耳群、官道口群、新元古界栾川群、下古生界陶湾群）；5—超大型钼(钨)矿床；6—大型钼(钨)矿床；7—中型钼矿床；8—铅锌银矿床；9—金（银铅）矿床；10—多金属硫铁矿床
Figure 5. Gravity and magnetic inferred hidden rock mass map of the Nannihu ore concentration area
1-Depth 0～800 m buried rock mass range; 2- Depth 0.8～1.5km buried rock mass range; 3-Depth 1.5～3 km buried rock mass range; 4-Surrounding rock stratum (from the north to the south of the Mesoproterozoic Xiong'er Group and Guandaokou Group, Neoproterozoic Luanchuan Group, lower Paleozoic Taowan Group); 5-Superlarge molybdenum (tungsten) ore deposit; 6-Large molybdenum (tungsten) ore deposit; 7-Medium molybdenum deposit; 8-Lead zinc silver deposit; 9-Gold (silver-lead) deposit; 10-Polymetallic sulfur iron deposit
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图 6 南泥湖矿集区成矿模式图
F1—栾川断裂；F2—马超营断裂；Pz1R—下古生界二郎坪群；Pz1T—下古生界陶湾群；Pt3L—新元古界栾川群；Pt2G—中元古界官道口群；Pt2-3K—中新元古界宽坪群；Pt2X—中元古界熊耳群；Pt1Q—古元古界秦岭岩群；AR—太古宇太华群；1—深源浅成花岗岩；2—浅源深成花岗岩；3—斑岩型钼（钨）矿；4—斑岩-矽卡岩型钼（钨）矿；5—隐伏斑岩型钼（钨）矿；6—隐伏斑岩-矽卡岩型钼（钨）矿；7—（岩钟）斑岩型钼（钨）矿；8—（岩钟）斑岩-矽卡岩型钼（钨）矿；9—脉型铅锌银矿；10—脉型金（银铅）矿；11—斑岩-脉型钼矿
Figure 6. Metallogenic model of the Nannihu ore concentration area
F1- Luanchuan fault; F2- Machaoying fault; Pz1R- Paleozoic Erlangping Group; Pz1T- Lower Paleozoic Taowan Group; Pt3L- Neoproterozoic Luanchuan Group; Pt2G- Middle Proterozoic Guandaokou Group; Pt2-3K- Middle Proterozoic and Neoproterozoic Kuanping Group; Pt2X- Mesoproterozoic Xiong'er Group; Pt1Q- Paleoproterozoic Qinling rock Group; AR- The Archean Taihua Group; 1- Deep source shallow granite; 2- Shallow source deep granite; 3- Porphyry molybdenum (tungsten) ore; 4- porphyry−skarn type molybdenum (tungsten) ore; 5- Concealed porphyry molybdenum (tungsten) ore; 6- Buried porphyry−skarn type molybdenum (tungsten) ore; 7- (Kupola) porphyry molybdenum (tungsten) ore; 8- (Kupola) porphyry−skarn type molybdenum (tungsten) ore; 9- Vein type lead-zinc-silver ore; 10- Vein type gold-(silver-lead) ore; 11- Porphyry−vein type molybdenum ore
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