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    Volume 45 Issue 1
    Jan.  2020
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    Liu Yongjun, Han Xiaotao, Liu Zhenghong, Wu Wenbin, Wang Yuping, Li Haiyang, Wang Xiaoliang, 2020. Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Early Cretaceous Granites in Fengcheng Area, Eastern Liaoning Province. Earth Science, 45(1): 145-155. doi: 10.3799/dqkx.2018.278
    Citation: Liu Yongjun, Han Xiaotao, Liu Zhenghong, Wu Wenbin, Wang Yuping, Li Haiyang, Wang Xiaoliang, 2020. Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Early Cretaceous Granites in Fengcheng Area, Eastern Liaoning Province. Earth Science, 45(1): 145-155. doi: 10.3799/dqkx.2018.278

    Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Early Cretaceous Granites in Fengcheng Area, Eastern Liaoning Province

    doi: 10.3799/dqkx.2018.278
    • Received Date: 2018-07-20
    • Publish Date: 2020-01-15
    • The magmatic rocks, which is widely distributed in Fengcheng area, Liaodong peninsula, is always a hot spot for study of North China Craton (NCC) thinning in recent years. However, due to lack of precise age and geochemical constraints in previous research, its petrogenesis and tectonic setting still remain controversial. In this paper, three granite plutons were studied by the petrology, petrogechemistry and LA-ICP-MS zircon U-Pb ages. The Maokuishan monzogranite, Jiaoyangyu granodiorite and Qingliangshan monzogranite were emplaced with the ages of 127.2±0.6 Ma, 122.9±1.1 Ma and 129.0±0.8 Ma, respectively. These granites were all constrained to Early Cretaceous. The zircons of granites have the characteristics of oscillatory growth zonation and high ratios of Th and U (Th/U>0.4), indicating a magmatic origin for the zircons. Geochemical characteristics suggest that Maokuishan and Qingliangshan monzogranites are both metaluminum A-type and peraluminous high-K calc alkaline granites, and the major elements are characterized by high Si, alk and low Al, Fe, Ca and Mg. The chondrite-normalized REE patterns have a moderate negative Eu anomalies. Jiaoyangyu granodiorites are metaluminum-peraluminous granodiorites, and the trace elements are enriched in Nd, Tb, La, and depleted in Sr, P, Ti. Combined with geological background, the three granite plutons in Fengcheng area discussed above were all formed in anorogenic extensional tectonic setting during Early Cretaceous, and also is the epitome of the lithosphere thinning and cratonic destruction of the North China Craton.

       

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