桂东大瑶山南缘社山花岗闪长岩的锆石U-Pb年龄及Hf同位素特征:对区内加里东期成岩成矿作用的制约
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摘要
利用激光剥蚀(MC)-ICP-MS方法对桂东大瑶山南缘的社垌钨钼矿床中的花岗岩类进行研究,精确限定社山黑云母花岗闪长岩(SD256)中锆石的206Pb/238 U加权平均年龄为438.7±3.0Ma(MSWD=0.22),侵位于平头背石英砂岩的花岗闪长(斑)岩脉(SD190)形成于438.1±2.6Ma(MSWD=0.28);花岗岩中新生岩浆锆石的Hf同位素特征较为一致,176 Hf/177 Hf比值分布于0.282 406~0.282 518,对应的εHf(438Ma)值变化于-3.7~0,两阶段Hf模式年龄(TDM2)集中在1 226~1 417Ma之间.这表明大瑶山地区社山花岗闪长岩类的形成时间在438Ma左右(加里东期),成岩成矿作用可能与中元古代新生地壳物质(1.2~1.4Ga)的部分熔融密切相关.结合区域内已有可靠年龄进行分析,认为华南加里东期成岩成矿作用应该不是呈简单的北东向分布,而是呈面状展布,且该期构造-岩浆-成矿运动可能是引起华南地区在印支期、燕山早期发生大规模的岩浆作用和金属成矿作用的关键原因之一.
In this paper,we present laser ablation(MC)-ICP-MS U-Pb dating and Hf isotopic compositions of zircons from two representative granitoid samples collected from Shedong W-Mo deposit in the southern edge of the Dayaoshan.Highly precise U-Pb results indicate that zircons from Sheshan biotite granodiorite(SD256)and granodiorite-(porphyry)(SD190)which emplaced in the Pingtoubei quartz sandstone yields weighted mean 206Pb/238 U age of 438.7±3.0Ma(MSWD=0.22)and 438.1±2.6Ma(MSWD=0.28),respectively.And the zircons crystallized in the Kwangsian granites yield 176 Hf/177 Hf ratios of0.282 406 to 0.282 518,εHf(438Ma)values ranging from-3.7to 0and Hf model ages(TDM2)of 1 226 to 1 417 Ma.Our U-Pb and Hf isotopic data can be interpreted as the crystallization time of granites,and indicate that it was formed in the~438Ma(Caledonian)and may have been formed by reworking of Mesoproterozoic juvenile crust(1.2-1.4Ga)closely related to partial melting.Together with other published geochronological data,it is proposed that the late Early Paleozoic granites predominantly have a similar formation age and exhibit a planar-shaped distribution,rather than a north-east-strikingdistribution pattern in the hinterland of the South China.Moreover,the Caledonian tectonic-magmatic-metallogenic movement may be the one of key reasons for the large-scale magmatism and metal mineralization in the following tectonic episodes,such as Indosinian and Yanshanian in the South China.
In this paper,we present laser ablation(MC)-ICP-MS U-Pb dating and Hf isotopic compositions of zircons from two representative granitoid samples collected from Shedong W-Mo deposit in the southern edge of the Dayaoshan.Highly precise U-Pb results indicate that zircons from Sheshan biotite granodiorite(SD256)and granodiorite-(porphyry)(SD190)which emplaced in the Pingtoubei quartz sandstone yields weighted mean 206Pb/238 U age of 438.7±3.0Ma(MSWD=0.22)and 438.1±2.6Ma(MSWD=0.28),respectively.And the zircons crystallized in the Kwangsian granites yield 176 Hf/177 Hf ratios of0.282 406 to 0.282 518,εHf(438Ma)values ranging from-3.7to 0and Hf model ages(TDM2)of 1 226 to 1 417 Ma.Our U-Pb and Hf isotopic data can be interpreted as the crystallization time of granites,and indicate that it was formed in the~438Ma(Caledonian)and may have been formed by reworking of Mesoproterozoic juvenile crust(1.2-1.4Ga)closely related to partial melting.Together with other published geochronological data,it is proposed that the late Early Paleozoic granites predominantly have a similar formation age and exhibit a planar-shaped distribution,rather than a north-east-strikingdistribution pattern in the hinterland of the South China.Moreover,the Caledonian tectonic-magmatic-metallogenic movement may be the one of key reasons for the large-scale magmatism and metal mineralization in the following tectonic episodes,such as Indosinian and Yanshanian in the South China.
引文
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