Geochemistry and zircon SHRIMP U-Pb chronology of Xiaolingzi granite in the Anshan area
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P588.121 P597

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    Abstract:

    Zircon SHRIMP U-Pb age dating indicates that the Xiaolingzi granite in the Anshan area was emplaced during Early Cretaceous(130.2±2.7 Ma).It is enriched in SiO2, Na2O+K2O, TFeO/MgO, LREE, Zr, Nb and Y, and depleted in CaO, Ba and Sr, thus similar to the widely distributed Qianshan granite with the geochemical characteristics of A type granite in this area. It is suggested that the magmatic activity was related to an extension following the subduction of the paleo-Pacific Plate beneath eastern China.

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杜利林 杨淳 万渝生 宋彪 耿元生,2005,鞍山小岭子花岗岩地球化学及锆石SHRIMP年代学[J].岩石矿物学杂志,24(4):279~284. DU Li_lin~,YANG Chun~,WAN Yu_sheng~,2005,Geochemistry and zircon SHRIMP U-Pb chronology of Xiaolingzi granite in the Anshan area[J]. Acta Petrologica et Mineralogica,24(4):279~284.

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