滇中老街子Pb-Ag多金属矿床的成矿时代及成矿动力学背景探讨:来自硫化物Re-Os同位素证据
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摘要
滇中老街子Pb-Ag多金属矿床位于红河-哀牢山新生代富碱斑岩带的中段,是与富碱火山-岩浆热液密切相关的典型矿床。首次在该矿床深部发现70m宽的高Cu-Mo异常黄铁矿化蚀变正长斑岩和黄铁矿-辉钼矿矿脉(2073中段3#穿脉),认为该矿床深部存在明显的富碱斑岩-岩浆热液型铜-钼矿化叠加成矿作用。本文选取深部坑道内的辉钼矿-黄铁矿脉、黄铁矿-方铅矿脉和高Cu-Mo异常黄铁矿化蚀变正长斑岩进行辉钼矿-黄铁矿Re-Os同位素成矿年代研究,获得了辉钼矿Re-Os等时线年龄33.71±0.29Ma和加权平均值年龄33.99±0.22Ma,说明滇中老街子斑岩型铜-钼成矿作用时代为渐新世,与Cu-Mo异常黄铁矿化蚀变正长斑岩成岩年龄一致。黄铁矿的初始Os比值(0.3049~1.5549)及其γOs值(140.5~1126)指示老街子Pb-Ag多金属矿床金属成矿物质主要来源于壳幔相互作用而形成的岩浆。老街子Pb-Ag多金属矿床成岩成矿年龄和区域上富碱斑岩-岩浆热液型多金属矿床成岩成矿年龄(30~40Ma)大致相当,表明印度板块与欧亚板块碰撞期后,构造应力场发生转变形成大规模区域左行走滑断裂系统,在稳定块体内部诱发壳幔过渡层发生部分熔融形成富碱岩浆和成矿流体,成矿流体沿着构造薄弱部位形成富碱斑岩-岩浆热液型多金属矿床。
The Laojiezi Pb-Ag deposit,located in the middle section of the Cenozoic Red River-Ailaoshan alkalirich porphyry belt,is the typical alkali-rich volcanic-magmatic hydrothermal deposit in central Yunnan province.A 70-m-wide syenite porphyry and molybdenite-pyrite vein with high Cu-Mo abnormal pyritization was firstly discovered in the deep part of the deposits(3# vein of 2073 level).It is believed that obvious alkali-rich porphyry and magmatic-hydrothermal Cu-Mo superimposed mineralization occurs at depth of the deposit.This study conducted Re-Os isotopic analysis for molybdenite-pyrite samples from molybdenite-pyrite veins,pyrite-galena veins and high Cu-Mo syenite porphyry from deep adits in the Laojiezi Pb-Ag deposits.An isochron age of 33.71± 0.29 Ma and a weighted average age of 33.99±0.22 Ma were obtained for molybdenite,indicating that the mineralization of the Pb-Ag polymetallic deposit took place in Oligocene,which is consistent with the diagenetic age of the syenite porphyry.The initial Os value of 0.3049～1.5549 and theγOsvalue of 140.5～1126 suggest that the metallogenic material was derived from partial melting of the crust-mantle transition layer.The metallogenic age of the Laojiezi porphyry Pb-Ag polymetallic deposit is roughly the same as that(30～40 Ma)of regional alkali-rich porphyry and magmatic hydrothermal polymetallic deposits.It shows that,after the collision between the India plate and Eurasia plate,the change of tectonic stress field resulted in large-scale strike-slip faulting system,which induced partial melting of crust-mantle transition zone within the stable cratons,forming alkali-rich intrusive rocks and metallogenic fluids,and the fluid formed alkali-rich porphyry and magmatichydrothermal polymetallic deposits along the weak structures.
The Laojiezi Pb-Ag deposit,located in the middle section of the Cenozoic Red River-Ailaoshan alkalirich porphyry belt,is the typical alkali-rich volcanic-magmatic hydrothermal deposit in central Yunnan province.A 70-m-wide syenite porphyry and molybdenite-pyrite vein with high Cu-Mo abnormal pyritization was firstly discovered in the deep part of the deposits(3# vein of 2073 level).It is believed that obvious alkali-rich porphyry and magmatic-hydrothermal Cu-Mo superimposed mineralization occurs at depth of the deposit.This study conducted Re-Os isotopic analysis for molybdenite-pyrite samples from molybdenite-pyrite veins,pyrite-galena veins and high Cu-Mo syenite porphyry from deep adits in the Laojiezi Pb-Ag deposits.An isochron age of 33.71± 0.29 Ma and a weighted average age of 33.99±0.22 Ma were obtained for molybdenite,indicating that the mineralization of the Pb-Ag polymetallic deposit took place in Oligocene,which is consistent with the diagenetic age of the syenite porphyry.The initial Os value of 0.3049～1.5549 and theγOsvalue of 140.5～1126 suggest that the metallogenic material was derived from partial melting of the crust-mantle transition layer.The metallogenic age of the Laojiezi porphyry Pb-Ag polymetallic deposit is roughly the same as that(30～40 Ma)of regional alkali-rich porphyry and magmatic hydrothermal polymetallic deposits.It shows that,after the collision between the India plate and Eurasia plate,the change of tectonic stress field resulted in large-scale strike-slip faulting system,which induced partial melting of crust-mantle transition zone within the stable cratons,forming alkali-rich intrusive rocks and metallogenic fluids,and the fluid formed alkali-rich porphyry and magmatichydrothermal polymetallic deposits along the weak structures.
引文
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