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    Volume 47 Issue 8
    Sep.  2022
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    Article Navigation >  Earth Science  > 2022  >  47(8): 2951-2967
    Li Tongyu, Jin Chao, Tian Zhonghua, Wang Wei, Hao Zhixuan, Wen Fei, 2022. Hf Isotopic and Geochronological Characteristics of Mesozoic Granites and Xenoliths in Rushan Area and Its Implication on Crustal Evolution of Jiaodong Peninsula. Earth Science, 47(8): 2951-2967. doi: 10.3799/dqkx.2021.154
    Citation: Li Tongyu, Jin Chao, Tian Zhonghua, Wang Wei, Hao Zhixuan, Wen Fei, 2022. Hf Isotopic and Geochronological Characteristics of Mesozoic Granites and Xenoliths in Rushan Area and Its Implication on Crustal Evolution of Jiaodong Peninsula. Earth Science, 47(8): 2951-2967. doi: 10.3799/dqkx.2021.154
    shu

    Hf Isotopic and Geochronological Characteristics of Mesozoic Granites and Xenoliths in Rushan Area and Its Implication on Crustal Evolution of Jiaodong Peninsula

    doi: 10.3799/dqkx.2021.154
    • 1.

      School of Earth Sciences and Engineering, Heibei University of Engineering, Handan 056038, China

    • 2.

      Key Laboratory for Resource Exploration Research of Hebei Province, Handan 056038, China

    • 3.

      Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 4.

      Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100029, China

    • Received Date: 2021-06-30
    • Publish Date: 2022-09-25
      Abstract
    • Granite is the main component of continental crust, and the occurrence of Mesozoic granite in Jiaodong Peninsula is an important basis for deducing magmatic evolution and tectonic evolution of subduction plates. Therefore, the study of granite and its xenoliths (meta⁃maficrocks) exposed in Rushan area is helpful to better understand the magmatic evolution and crustal evolution of Jiaodong Peninsula in Mesozoic. This study provides new data of major and traceelements, U⁃Pb dataand Lu⁃Hf isotopesfor Jiaodong Peninsula. Petro⁃geochemistry shows that the biotite monzogranite has the characteristics of high potassium and calcium alkalinity, and is relatively poor in elements such as titanium, iron, manganese, and magnesium. The rock may be I⁃type or M⁃type granite with a high degree of differentiation.The large ion lithophile elements Ba and Sr are obviously enriched, and the high field strength element Zr has no obvious loss.The SiO2, TiO2, Fe2O3T, and MgO content of the amphibolite are 48.9%, 0.68%, 12.64% and 7.33%, respectively. It is a tholeiitic basalt composition, and the total alkali ALK (K2O+Na2O) is relatively low.The large ion lithophile elements Ba and Sr are not significantly enriched, and the high field strength element Zr is weakly depleted, which is similar to the geochemical properties of the garnet plagioclase amphibolite.The granite has magmatic zircon and the amphibolite contains metamorphic recrystallized zircon under zircon CL image. The zircon U⁃Pb dating age of the biotite monzogranite is 118.5±2.7 Ma, and the value of εHf(t) is -15.4 to -27.7 (Mean=-25.2±1.4), and the corresponding two⁃stage model age (TDM2) is 2.16 to 2.90 Ga, but most of them are concentrated in ~2.8 Ga.The upper intersection age amphibolite(xenoliths) is 1 839±27 Ma(zircon U⁃Pb), and and the value of εHf(t) is 0.5 to 5.1 (Mean=3.23±0.74), corresponding to the one⁃stage model age (TDM1) is 2.02 to 2.18 Ga.In addition, the value of εHf(t) of the granite⁃bearing granite in Niantou Village is -25.1 to -27.1 (Mean=-26.0±0.18), and the corresponding two⁃stage model age (TDM2) is 2.75 to 2.87 Ga.The εHf(t) value of the xenoliths (garnet amphibolite) is 3.7 to 4.4 (Mean=3.93±0.21), and the corresponding one⁃stage model age (TDM1) is 1.99 to 2.03 Ga.The above data indicate that the granite is the product of Archean crust remelting in the Eastern North China Craton; the meta⁃mafic rocks can be classified into the Jingshan Group of the North China Craton.Therefore, the Mesozoic granite and its xenoliths in the Rushan area have the same affiliation as the North China Craton. The granites with model ages of Archean age in the Rushan area suggest information about the crustal evolution of the Jiaodong Peninsula. It does not have the characteristics of magmatic rock produced by delamination. A short time after partial melting of the lower crust entrained, many ancient xenoliths (meta⁃mafic rocks) were carried to the subsurface by re⁃melting magma.

       

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