Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 587-625.doi: 10.13278/j.cnki.jjuese.20170179

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Age, Petrogenesis and Their Constraints on Regional Crustal Evolution of Late Neoarchean Gneisses in Southeast Jilin Province

Wang Chaoyang1, Meng En1, Li Zhuang2, Li Yanguang3, Jin Mengqi3   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
    2. College of Geosciences, China University of Petroleum, Beijing 102249, China;
    3. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
  • Received:2017-12-20 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41572169, 40725007, 41202136) and Project of China Geological Survey (12120114021601, 12120114021401, 12120114061901)

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Abstract: The Early Precambrian granitic gneiss are widely distributed in Tonghua in southeast Jilin Province. The lithological assemblages, ages and petrogenesis of these granitic gneiss are informative to the formation and evolution of the early crust in the northeastern margin of the North China craton. Based on the systematic petrology, zircon U-Pb chronology, element and Lu-Hf isotopic geochemistry results, we divided these granitic gneisses into high silicon group and low silicon group according to their SiO2 contents. The former is mainly composed of monzogranite gneisses, trondhjemite gneisses and tonalite gneisses, and the magmatic precursors was emplaced at 2 549-2 557 Ma. While the latter is composed of quartz-monzonitic diorite gneisses and granodiorites gneisses, and their protolith may be formed at 2 534-2 552 Ma. The both groups contain zircons captured at ca. 2 600 Ma, and suffered from the metamorphism for ca. 2 500 Ma. The geochemical data show that the low silicon group is rich in MgO, CaO and Na2O, belonging to the high-medium K calc-alkaline series, and has the feature of higher contents of LREE, but lower contents of HREE and HFSE. In contrast, the high silicon group has the lower MgO and CaO, and exhibit a stronger fractionation between the light and heavy rare earth elements, and the elements of Nb, Ta, P, Ti are depleted. The two groups show the weak positive or negative Eu anomalies. In combination with the regional geological data in this study, we believe that the two groups were derived from the same source, and their formation may be related to the ocean plate subduction through a partial melting of the crust caused by the magma underplating. Moreover, the two groups have similar εHf(t) values (2.72 to 7.95) and model age (2.86 to 2.55 Ga), which suggests that a crustal growth occurred in the study area in the Late Neoarchean. According to the research progress of metamorphic volcanic rocks in the region, we consider that the granitic gneisses in Tonghua may be formed at an active continental margin.

Key words: southeast Jilin Province, granitic gneisses, Late Neoarchean, geochemistry, petrogenesis

CLC Number: 

  • P588.345
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