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    Volume 45 Issue 12
    Dec.  2020
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    Article Navigation >  Earth Science  > 2020  >  45(12): 4589-4603
    Liao Fengyun, Chen Wei, Cao Xiaofeng, Chen Guangchen, He Kunyang, Yang Wen, Wu Yibu, Li Tongguo, 2020. Petrogenesis and Forming Environment of Monzonitic Granite in Yushishan Nb-Ta Mining Area, Akesai, Gansu Province:Evidences from Chronology and Geochemistry. Earth Science, 45(12): 4589-4603. doi: 10.3799/dqkx.2019.260
    Citation: Liao Fengyun, Chen Wei, Cao Xiaofeng, Chen Guangchen, He Kunyang, Yang Wen, Wu Yibu, Li Tongguo, 2020. Petrogenesis and Forming Environment of Monzonitic Granite in Yushishan Nb-Ta Mining Area, Akesai, Gansu Province:Evidences from Chronology and Geochemistry. Earth Science, 45(12): 4589-4603. doi: 10.3799/dqkx.2019.260
    shu

    Petrogenesis and Forming Environment of Monzonitic Granite in Yushishan Nb-Ta Mining Area, Akesai, Gansu Province:Evidences from Chronology and Geochemistry

    doi: 10.3799/dqkx.2019.260
    • 1.

      School of Earth Resources, China University of Geosciences, Wuhan 430074, China

    • 2.

      National Demonstration Center for Experimental Mineral Exploration Education, China University of Geosciences, Wuhan 430074, China

    • 3.

      Gansu Geological Survey, Lanzhou 730000, China

    • Received Date: 2019-07-24
    • Publish Date: 2020-12-15
      Abstract
    • The Yushishan Nb-Ta mining area is located at the junction of North Altun, Qaidam and Qilian, and the tectonic evolution of this area is complex. The research of petrology, rock geochemistry, zircon U-Pb chronology and zircon Lu-Hf isotope was carried out on the monzonitic granite to reveal petrogenesis and forming environment of it. The detailed name of the monzonitic granite is medium-fine-grained porphyritic biotite monzonitic granite and its dark minerals are mainly biotite and hornblende. The geochemical characteristics show that the monzonitic granite belongs to the typical high-K series with quasi-aluminous to weakly peraluminous. Large ion lithophile elements (Rb, Th and K) are relatively enriched and high field strength elements (Nb, Sr, P and Ti) are in distinct negative anomaly. The REE distribution patterns show negative Eu anomaly, with the mean δEu value of 0.57 and the mean (La/Yb)N value of 11.09, they show that the monzonitic granite magma has a high degree of partial melting. The features of petrological and geochemical indicate that the monzonitic granite belongs to I-type granite. Zircon LA-ICP-MS U-Pb dating of the monzonitic granite yielded a crystallization age of 481.3±1.7 Ma and it was formed in the Early Ordovician. The zircons Lu-Hf isotope analysis shows that the εHf(t) ranges from +0.4 to +11.8 and the two-stage Hf model ages range from 675 to 1 308 Ma, suggesting that the source rocks are partial melting of Neoproterozoic juvenile crustal materials. The formation of the monzonitic granite was closely related to that North Altun oceanic crust subducted Middle-South Qilian continental crust, in the Yushishan area on the edge of Middle-South Qilian continental crust (back arc), the upward intrusion of molten magma from the fractures formed the monzonitic granite because of the subduction of the oceanic crust.

       

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