Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (6): 1589-1619.doi: 10.13278/j.cnki.jjuese.201706101

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Geochronology, Petrogenesis and Constraints on Regional Tectonic Evolution of the Meta-Volcanic Rocks in Southeastern Liaodong Peninsula

Meng En1, Wang Chaoyang1, Liu Chaohui1, Shi Jianrong2, Li Yanguang3   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
    2. Tianjin Center of Geological Survey, China Geological Survey, Tianjin 300170, China;
    3. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
  • Received:2017-09-23 Online:2017-11-26 Published:2017-11-26
  • 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 Paleoproterozoic meta-supracrustal rocks, known as the South Liaohe Group, is widely exposed in the southeast of Liaodong Peninsula. Its lower part is characterized by the extensive metavolcanic rocks. In this paper, we study the petrology and whole-rock geochemical data of the biotite plagioclase gneiss, amphibolite, and biotite leptynites, as well as the U-Pb dating and Lu-Hf isotope data of the zircons in these rocks. The aim is to restrict the petrogenesis of Jiao-Liao-Ji belt by researching their composition, the ages of formation and metamorphism of the protolith, and the petrogenesis. The structure, composition, and U-Pb ages of zircon indicate that the protoliths of the metavolcanic rocks in South Liaohe Group were formed at ca. 2.19 Ga, and they were affected by metamorphic events at 1.90 Ga. The element and isotope geochemical analysis show that the protoliths of these rocks were basaltic andesite-andesite, dacite, and minor rhyolite; most of them belong to sub-alkaline affinities with calc-alkaline evolution. The basic rocks have relatively low SiO2 contents, enriched in MgO, TFe2O3, and light rare-earth elements(LREE), Cr, Co, and Ni, while depleted of heavy rare-earth elements(HREE) and high-field strength elements(HFSE, such as Nb, Ta and Ti), indicating a derivation from a partial melting of a depleted lithospheric mantle that had been altered by the fluids or melts derived from a subducted slab. However, the intermediate acid rocks have high contents of SiO2 and low contents of MgO and TFe2O3, enriched in alkalis, Ba, Th, U and K, while depleted of Nb, Ta, P and Ti, indicating that the acidic rocks could have been derived from a partial melting of juvenile crust. Taking into account the regional geology, we consider that the metavolcanic rocks of the South Liaohe Group formed under an active continental margin, and the evolution of the northern segment of the Jiao-Liao-Ji belt was related to an arc-continent collision before the middle Paleoproterozoic.

Key words: Paleoproterozoic South Liaohe Group, metavolcanic, petrogenesis, tectonic setting, Jiao-Liao-Ji belt

CLC Number: 

  • P588.3
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