阳春盆地陂头面铜多金属矿床成岩成矿年代学、锆石微量元素及地质意义
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摘要
广东陂头面铜多金属矿位于云开地区的阳春盆地内,是一个与中细粒花岗闪长岩有关的矽卡岩型矿床。矿体形态不规则,主要呈层状、似层状和透镜状,受NE和NNE向构造断裂控制。本文在详细了解矿床地质特征的基础上,通过LAICP-MS锆石U-Pb测年以及辉钼矿Re-Os同位素定年技术首次对陂头面矿床进行了成岩成矿年代学研究。成矿岩体花岗闪长岩的锆石U-Pb等时线年龄为163. 5±0. 55Ma,4件辉钼矿样品的模式年龄为162. 9～163. 9Ma,加权平均值为163. 3±1. 1Ma,结果表明陂头面铜多金属矿床成岩成矿作用基本同时发生于中侏罗世晚期,这也是阳春盆地首次报道的形成于该时期的多金属矿床。该矿床辉钼矿样品的Re含量变化于30. 5×10~(-6)～41. 7×10~(-6),表明其成矿物质具有壳幔混源的特征。本文对成矿岩体开展了锆石微量元素的详细研究,结果获得锆石CeⅣ/Ⅲ比值范围为198～987,表明其具有高的氧逸度和很好的成矿潜力;锆石Ti饱和温度为597～782℃,暗示可能形成于与俯冲作用有关的构造环境。陂头面铜多金属矿床成岩成矿年龄的确定为下一步在阳春盆地及区域上开展150～170Ma左右的斑岩-矽卡岩多金属矿床找矿勘探提供了重要的线索,也为进一步深入研究钦杭成矿带成岩成矿作用动力学背景提供了新的资料。
The Potoumian Cu polymetallic deposit,located in Yangchun basin of Yunkai area,is a skarn deposit related to mediumto fine-grained granodiorite. The ore bodies mainly occurred as lamellar,stratiods and lenses in shape,controlled by NE and NNEstriking faults. In this study,we present detailed geologic characteristics of the deposit and carried out chronological studies of LA-ICPMS zircon U-Pb ages for the ore-bearing granitoids and molybdenite Re-Os ages for the Potoumian deposit. Zircon U-Pb analyses yields an age of 163. 5 ± 0. 55 Ma for the medium-to fine-grained granodiorite. Precise Re-Os dating of molybdenite shows that the Re-Os model ages of four samples range from 162. 9 Ma to 163. 9 Ma,with a weighted mean age of 163. 3 ± 1. 1 Ma. These dating results suggest that the timing for the granodiorite and Cu polymetallic mineralization are simultaneously formed in the late stages of the Middle Jurassic,which is firstly reported in the Yangchun basin. The rhenium content of molybdenite samples are in the range of 30. 5 × 10~(-6)~ 41. 7 × 10~(-6),implying that Cu and Mo were derived from the crust-mantle mixed source. The CeⅣ/Ⅲvalues of zircons in the granodiorite from the Potoumian Cu polymetallic deposit are from 198 to 987,which suggest that its magma has a high oxygen fugacity and good metallogenic potential. The forming temperature of the granodiorite calculated by zircon Ti thermometer are from 597℃ to782℃,indicating that its magma is probably closely related to a subducted environment. These results,together with geological records in South China,suggest that the formation of the Potoumian deposit is corresponding to the period of the large-scale mineralization in the Middle-Late Jurassic of South China. This highlights potential for discovery of additional deposits and extends the favorable interval for exploration for porphyry-skarn Cu polymetallic deposits around 170 ~ 150 Ma in the Yangchun basin,and also provides new information for further discussing on the geodynamic settings of the Qin-Hang metallogenic belt.
The Potoumian Cu polymetallic deposit,located in Yangchun basin of Yunkai area,is a skarn deposit related to mediumto fine-grained granodiorite. The ore bodies mainly occurred as lamellar,stratiods and lenses in shape,controlled by NE and NNEstriking faults. In this study,we present detailed geologic characteristics of the deposit and carried out chronological studies of LA-ICPMS zircon U-Pb ages for the ore-bearing granitoids and molybdenite Re-Os ages for the Potoumian deposit. Zircon U-Pb analyses yields an age of 163. 5 ± 0. 55 Ma for the medium-to fine-grained granodiorite. Precise Re-Os dating of molybdenite shows that the Re-Os model ages of four samples range from 162. 9 Ma to 163. 9 Ma,with a weighted mean age of 163. 3 ± 1. 1 Ma. These dating results suggest that the timing for the granodiorite and Cu polymetallic mineralization are simultaneously formed in the late stages of the Middle Jurassic,which is firstly reported in the Yangchun basin. The rhenium content of molybdenite samples are in the range of 30. 5 × 10~(-6)~ 41. 7 × 10~(-6),implying that Cu and Mo were derived from the crust-mantle mixed source. The CeⅣ/Ⅲvalues of zircons in the granodiorite from the Potoumian Cu polymetallic deposit are from 198 to 987,which suggest that its magma has a high oxygen fugacity and good metallogenic potential. The forming temperature of the granodiorite calculated by zircon Ti thermometer are from 597℃ to782℃,indicating that its magma is probably closely related to a subducted environment. These results,together with geological records in South China,suggest that the formation of the Potoumian deposit is corresponding to the period of the large-scale mineralization in the Middle-Late Jurassic of South China. This highlights potential for discovery of additional deposits and extends the favorable interval for exploration for porphyry-skarn Cu polymetallic deposits around 170 ~ 150 Ma in the Yangchun basin,and also provides new information for further discussing on the geodynamic settings of the Qin-Hang metallogenic belt.
引文
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