Ages of Cishan granite in Yantai, Jiaodong, and their metallogenic implications
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P588.121 P597

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    Abstract:

    The U-Pb ages of zircon from Cishan granite were determined by LA-ICP-MS (Laser ablation-inductively coupled plasma_mass spectrometer). The ages of 199~149 Ma from 8 grains indicate the Jurassic formation of the granite, which can thus be termed Yanshanian granite. The ages of 2 110~2?467 Ma (2 252±41 Ma in average) from 4 grains of Early Paleozoic inherited zircon show that the source of the granite contains materials from Early Paleozoic Fenzishan Group. The formation ages of the granite provide important evidence for the origin of the Nanzhangjia gold deposit.

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孟繁聪 史仁灯 Tsuyoshi Iizuka 杨经绥 Takafumi Hirata,2005,胶东烟台磁山花岗岩的形成时代及其成矿意义[J].岩石矿物学杂志,24(5):464~468. MENG Fan-cong~,SHI Ren-deng~,Tsuyoshi Iizuka~,YANG Jing-sui~,Takafumi Hirata~,2005,Ages of Cishan granite in Yantai, Jiaodong, and their metallogenic implications[J]. Acta Petrologica et Mineralogica,24(5):464~468.

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  • Received:July 05,2005
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