Metallogenic law and exploration prospect of the middle part of Nanling metallogeny belt
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摘要:
研究目的 南岭中段是中国重要的有色金属、能源矿产、非金属和水气矿产资源基地，成矿地质条件优越、矿产类型丰富、成矿作用类型复杂，深入理解其成矿规律是开展区域成矿理论研究和实现找矿突破的关键。
研究方法 本文基于前人丰硕的成果资料，对南岭成矿带中段成矿规律和找矿方向进行了总结分析。
研究结果 此次研究明确了南岭中段主要控矿地质条件，厘定了区域两种构造格架体系的控矿作用；依据矿产资源特征，总结了成矿特征、规律及其演化，进一步探讨了区域岩浆演化和成矿潜力；整理出了南岭成矿带中亚带目前发育的50个矿种、872处矿产地和15种矿床类型，并探讨了主成岩作用特征、演化及其成矿潜力。
结论 南岭中段找矿的主攻方向为：寻找接触带附近的铀矿、煤矿的滑覆构造、受变质和硫铁矿区风化型铁矿、有色金属组合的综合预测和寻找缺位类型，寻找新类型稀有、稀散矿和独立金矿，保护和开发伴生宝石矿。围绕着骑田岭及周边、乐昌—韶关—翁源远景区，有望实现钨锡钼铋铜铅锌铀稀土等矿产的找矿突破。
Abstract:This paper is the result of mineral exploration engineering.
Objective The middle part of Nanling metallogeny belt, an important resource base of non–ferrous metal, energy minerals, non–metallic minerals, groundwater and gas minerals, has superb metallogenic geological conditions, abundant mineral types and complex mineralization types. In depth understanding of the metallogenic law is the key to carry out regional metallogenic theory research and to achieve prospecting breakthrough.
Methods In this paper, the metallogenic regularity and prospecting direction of the middle part of Nanling metallogenic belt are summarized and studied on the basis of the abundant previous data.
Results The main ore–controlling geological conditions are identified and the two ore–controlling structure frameworks are determined in the middle part of Nanling metallogeny belt. Depending on the characteristics of mineral resources, the metallogenic characteristics, rules and evolution are summarized, and regional magmatic evolution and metallogenic potential are further discussed. Moreover, 50 minerals, 872 ore deposits and 15 deposit types developed in the middle part of Nanling metallogeny belt are sorted out, and the predominant magmatism characteristics, evolution and metallogenic potential are discussed.
Conclusions The prospecting of the middle part of Nanling metallogeny belt should be focused on: comprehensive prediction of U ore near the contact zone, sliding overburden structure of coal mine, metamorphic and weathering type Fe ore in pyrite mining areas, comprehensive prediction and exploration of missing types of non–ferrous metals, exploration new types of rare and scattered metals and independent Au ore, protection and exploitation the associated gem mine. Two important prospecting potential areas, which include Qitianling and its surrounding, and Lechang–Shaoguan–Wengyuan, are proposed for the key region for prospecting breakthrough of tungsten, tin, molybdenum, bismuth, copper, zinc, uranium, rare earth, etc.
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图 1 南岭成矿带区域构造概略图（a，据陈毓川等, 1989; 徐志刚等, 2008）和地质图（b，据黄崇轲等, 1997）
Figure 1.
图 4 南岭成矿带中段岩浆岩Rb–Ba–Sr图解（a）、(Zr+Nb+Y)–Rb/Ba图解（b）、Zr/Hf–Nb/Ta图解（c）和K/Rb–Nb/T图解（d）
Figure 4.
表 1 南岭成矿带中段主要花岗岩体年龄
Table 1. Formation age of main granitic plutons in the middle part of Nanling metallogeny belt
岩体 岩性 时代 方法 参考文献 石背 黑云母二长花岗岩 174.3~187.5 Ma LA–ICP–MS 程顺波等, 2016; 林小明等, 2016 锡田 细粒黑云花岗岩、花岗岩、黑云二长花岗岩 147~151.7 Ma、
（228.5±2.5）MaLA–ICP–MS、SHRIMP、SIMS 马铁球等, 2005; 刘国庆等, 2008; 付建明等, 2012; 周云等, 2013; 陈迪等, 2014 贵东 二云母花岗岩、黑云母二长花岗岩 151~189.1 Ma、
228~239 MaLA–ICP–MS、SIMS、SHRIMP 孙涛等, 2003; 徐夕生等, 2003; 吴继光, 2013; 李建华等, 2014; 单芝波, 2014;
林坤等, 2021宝山 花岗闪长斑岩 156.3~164.1 Ma LA–ICP–MS、SIMS 伍光英等, 2005; 路远发等, 2006; 谢银财, 2013; 弥佳茹等, 2018 大坊 花岗闪长岩 （154.5±1.0）Ma LA–ICP–MS 弥佳茹等, 2018 水口山 英安斑岩、花岗闪长岩 148.8~173 Ma LA–ICP–MS、SHRIMP 甄世民等, 2012; 左昌虎等, 2014; 李永胜等, 2015 大义山 黑云母二长花岗岩、二云母二长花岗岩 147.5~171.8 Ma LA–ICP–MS 塔山 黑云母二长花岗岩、二云母二长花岗岩 218~247 Ma LA–ICP–MS 李勇等, 2015;
郭爱民等, 2017邓埠仙 白云母碱长花岗岩 154.4~158.6 Ma、
218.2~230 MaLA–ICP–MS 汪群英等, 2015;
陈迪等, 2017骑田岭 角闪黑云二长花岗岩、细粒黑云母花岗岩 141~160 Ma LA–ICP–MS 毛景文等, 2004; 付建明等, 2004; 马丽艳等, 2005; 柏道远等, 2005; 李华芹等, 2006 黄沙坪 花岗斑岩、石英斑岩 82.9~179.9 Ma SHRIMP 姚军明等, 2005; 王登红等, 2010; 全铁军等, 2012 界牌岭 花岗斑岩 90.5~92 Ma LA–ICP–MS 王登红等, 2010 香花岭—癞子岭 黑云母碱长花岗岩、黄玉霏细斑岩香花岭岩、细粒花岗岩 150.37~151.18 Ma LA–ICP–MS 来守华, 2014 瑶岗仙 斑状花岗岩、白云母花岗岩 157~170.7 Ma LA–ICP–MS 董少花等, 2014 大东山 黑云母二长花岗岩、黑云母钾长花岗岩 155.9~165 Ma LA–ICP–MS 张敏等, 2003; 黄会清等, 2008; 程亮开, 2018 热水 钾长花岗岩、黑云母花岗岩 （162.8±5.8）Ma SHRIMP 邓平等, 2011 王仙岭 黑云母二长花岗岩、白云母花岗岩 （155.9±1.0）Ma、
224~235 MaLA–ICP–MS 郑佳浩和郭春丽, 2012; Zhang et al., 2015 湖南桂东 花岗闪长岩、角闪黑云母花岗岩 （148.2±1.7）Ma、
（207.5±2.7）Ma、
（414.5±4.5）MaLA–ICP–MS 王登红等, 2010 五峰仙 黑云母二长花岗岩、二云母二长花岗岩 （230.8±1.7）Ma LA–ICP–MS 王凯兴等, 2012 连阳−白浆 斑状黑云二长花岗岩 100~102 Ma、
（144.3±0.8）MaLA–ICP–MS 高剑峰等, 2005;
马星华等, 2014千里山 斑状黑云母花岗岩、花岗斑岩 （152±2）Ma SHRIMP Li et al., 2004 
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表 2 南岭成矿带中段矿种及其矿产地数量
Table 2. Mineral species and number of mineral sites of the middle part of Nanling metallogeny belt
矿种 矿产地/处 矿种 矿产地/处 矿种 矿产地/处 白云岩 4 脉石英 2 石墨 5 铋 4 煤 77 石英岩 2 冰洲石 2 锰 75 水晶 10 大理岩 14 钼 6 锑 24 地热 69 耐火黏土 6 天然矿泉水 16 地下水 12 泥炭 2 天然石英砂 2 高岭土 3 铌钽 6 铁 145 汞 1 硼矿物 3 铜 12 硅灰石 3 膨润土 1 钨 44 红柱石 1 铍 2 稀土 15 花岗岩 3 其他黏土 8 锡 56 滑石 5 铅锌 104 页岩 1 金 6 铷 2 萤石 12 金红石 1 砂岩 4 铀 20 磷 1 砷 2 长石 1 硫铁矿 24 石膏 4 重晶石 4 铝 1 石灰岩 45
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表 3 南岭成矿带中段矿床主要成矿特征
Table 3. Main mineralization characteristics of the deposits in the middle part of Nanling metallogeny belt
成矿作用 矿床类型 矿产地数量 主要矿种 主要成矿期 典型矿床 （内生）
岩浆作用岩浆型矿床 4 花岗岩、铌钽 印支期、燕山期 小龙、垄上花岗岩矿、隘子铌钽矿 伟晶岩型矿床 3 铌钽 燕山期 531、隘子东、一六铌钽矿 云英岩型矿床 7 铌钽、锡 燕山期 尖峰岭铌钽矿、狮形岭锡矿 接触交代型矿床 101 钨、锡、钼、硅灰石、铅锌、大理岩、铁、硼、水晶 燕山期、（华力西期、前寒武纪） 黄沙坪铅锌矿、水底下、东风、朝天硅灰石矿、汤市硼矿、烟竹湖硼矿、大顶铁矿、谢家山锡矿、瑶田钨矿、大平锡矿、青石岩砷矿、大顶铁矿、大中山水晶矿、大顺窿铜矿、新田岭钨矿、一六、单竹坑钨矿 岩浆热液型矿床 197 钨、铷、锡、铍、铜、萤石、水晶、铀、重晶石、铋、
滑石、硫铁矿燕山期、（华力西期、印支期） 长岗岭铋矿、界滩滑石矿、锦潭硫铁矿、湘东铌钽矿、大笋、小坑铍矿、大尖山铅锌矿、田尾铅锌矿、拖碧塘铷矿、杉木溪铷矿、鸡脚山水晶矿、红岭、锯板坑、邓阜仙钨矿、天字号、芙蓉、白蜡水、香花岭锡矿、荷花坪锡矿、江口萤石矿、坪田铀矿、601铀矿、十里亭重晶石矿 （内生）
变质作用受变质型矿床 3 铁矿、石英岩 前寒武纪、燕山期、华力西期 九家坳铁矿、芝麻山铁矿、五官庙石英岩矿 变成型矿床 20 大理岩、石墨（红柱石、石英岩） 燕山期 鸡公岭、安源、三托坪、鲁塘、青坑、长江、大旺 （内生）
含矿流体作用浅成中—低温热液型矿床 54 铅锌、锑、铀、汞、硫铁矿、冰洲石 华力西期、燕山期、加里东期 红岩、西牛硫铁矿、西岸汞矿、赤佬顶锑矿、圆山、东城铀矿、高坳冰洲石矿 （外生）
表生作用风化型矿床 165 锰、稀土、铁、
高岭土、其他黏土喜山期 寨背顶稀土、来石稀土、大坪 （外生）
沉积作用机械沉积型矿床 16 砂岩、页岩、石英砂、黏土 喜山期、燕山期、华力西期 乌石砂岩、牛岭砂岩、红光页岩矿 化学沉积型矿床 94 白云岩、硫铁矿、
石灰岩、（铁、锰）华力西期、印支期 南头冲、柏塘、石灰岭、李家湾、罗仙岭、狮子山、燕山岭 生物化学沉积型矿床 80 煤矿、泥炭矿 华力西期、印支期 永耒煤矿、白沙煤矿、杨梅山煤矿、盘村泥炭矿 蒸发沉积型 4 石膏 喜山期、燕山期 星子盆地石膏矿 （外生）
流体作用流体型矿床 107 天然矿泉水、地热、地下水 喜山期 汤泉地热、地下水、宝林山矿泉水 叠加（复合/
改造）叠加（复合/改造）矿床 5 铀、铅锌、锰、铜、滑石 燕山期、华力西期、喜山期 水口山、杨柳塘、玛瑙山、大宝山、大莨
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表 4 南岭成矿带中段主要矿床成矿年龄
Table 4. Formation age of main deposits in the middle part of Nanling metallogeny belt
矿床名称 测试对象和测年方法 年龄/Ma 资料来源 石背大顶铁锡矿 金云母Ar–Ar 185.9±1.2 程顺波等, 2016 辉钼矿Re–Os 186.7±1.2 袁顺达, 2017 锡田锡钨矿 石英Rb–Sr 153±12 付建明等, 2012 辉钼矿Re–Os 150.0±2.7 刘国庆等, 2008 辉钼矿Re–Os 150.3±0.5 董超阁, 2018 宝山铅锌多金属矿 辉钼矿Re–Os 160±2 路远发等, 2006 三角潭钨矿 辉钼矿Re–Os 224.9±1.3 彭能立等, 2017 白沙子岭锡矿 石英Rb–Sr 160±1 张晓军等, 2014 邓阜仙钨矿 辉钼矿Re–Os 152.4±3.3 蔡杨等, 2012 白云母Ar–Ar 148.3±1.1 孙颖超等, 2017 辉钼矿Re–Os 150.7±2.3 董超阁, 2018 金船塘锡矿 矽卡岩矿物Sm–Nd 141±11 马丽艳等, 2010 黄铁矿Pb–Pb 164±12 肖红全等, 2003 辉钼矿Re–Os 158.8±6.6 刘晓菲, 2014 红旗岭锡多金属矿 石英Rb–Sr 143.1±8.7 马丽艳等, 2010 矿脉白云母Ar–Ar 153.5±1.5 袁顺达等, 2012 芙蓉白腊水锡矿 金云母Ar–Ar 154.1±1.1 彭建堂等, 2007 角闪石Ar–Ar 156.9±1.1 彭建堂等, 2007 芙蓉淘锡窝锡矿 白云母Ar–Ar 154.8±0.6 彭建堂等, 2007 芙蓉三门锡矿 白云母Ar–Ar 156.1±0.4 毛景文等, 2004 芙蓉淘锡窝锡矿 白云母Ar–Ar 160.1±0.9 毛景文等, 2004 芙蓉锡矿 含矿云英岩Rb–Sr 146±3 马丽艳等, 2005 芙蓉白腊水锡矿 石英Rb–Sr 177±39 蔡锦辉等, 2004 黄沙坪铅锌多金属矿床 矿脉辉钼矿Re–Os 153.8~157.5 马丽艳等, 2007; 毛景文等, 2007; 王登红等, 2010 香花岭锡多金属矿 白云母Ar–Ar 154.4±1.1 Yuan et al., 2007 香花岭—牛角湾 闪锌矿脉石英Rb–Sr 154±2 王登红等, 2010 闪锌矿脉萤石Sm–Nd 156.1±8.4 王登红等, 2010 香花岭—新风 黄铁矿Re–Os 158.9 王登红等, 2010 界牌岭锡多金属矿 矿脉黑云母Ar–Ar 91.1±1.1 毛景文等, 2007 白云母Ar–Ar 92.1±0.7 Yuan et al., 2015 瑶岗仙钨矿 辉钼矿Re–Os 158.0±1.2 李顺庭等, 2011 瑶岗仙尚滩钨矿 辉钼矿Re–Os 160.0±3.3 李顺庭等, 2011 瑶岗仙钨矿 石英Rb–Sr 175.8±4.1 王登红等, 2009 石英Rb–Sr 156±3 王登红等, 2009 辉钼矿Re–Os 170±5 王登红等, 2009 合江口锡矿 辉钼矿Re–Os 225.0±3.6 邓湘伟等, 2015 荷花坪锡矿 辉钼矿Re–Os 224.0±1.9 蔡明海等, 2006 锆石U–Pb 156 Zhang et al., 2015 香花铺钨矿 白云母Ar–Ar 161.3±1.1 Yuan et al., 2007 尖峰岭锡矿 白云母Ar–Ar 158.7±1.2 Yuan et al., 2007 桂东青石岭钨多金属矿 辉钼矿Re–Os 147.6±6.8 王登红等, 2010 下庄335铀矿 沥青铀矿U–Pb 93.5±1.2 邹东风等, 2011 下庄石土岭铀矿 沥青铀矿U–Pb 138.5±1.9 何德宝, 2017 下庄希望铀矿 沥青铀矿U–Pb 81.8±1.1 何德宝, 2017 下庄寨下铀矿 沥青铀矿U–Pb 92.0±1.3 何德宝, 2017 下庄仙石铀矿 沥青铀矿U–Pb 96.4±1.4 何德宝, 2017 下庄竹山下 沥青铀矿U–Pb 134 李子颖等, 2011 下庄大帽峰 沥青铀矿U–Pb 84.3 李子颖等, 2011 下庄仙人嶂 沥青铀矿U–Pb 81 李子颖等, 2011 柿竹园钨多金属矿 辉钼矿Re–Os 151.0±3.5 李红艳等, 1996 萤石Sm–Nd 149±2 Li et al., 2004
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