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    Volume 34 Issue 1
    Jan.  2009
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    ZHOU Xin-hua, YING Ji-feng, ZHANG Lian-chang, ZHANG Yu-tao, 2009. The Petrogenesis of Late Mesozoic Volcanic Rock and the Contributions from Ancient Micro-Continents: Constraints from the Zircon U-Pb Dating and Sr-Nd-Pb-Hf Isotopic Systematics. Earth Science, 34(1): 1-10.
    Citation: ZHOU Xin-hua, YING Ji-feng, ZHANG Lian-chang, ZHANG Yu-tao, 2009. The Petrogenesis of Late Mesozoic Volcanic Rock and the Contributions from Ancient Micro-Continents: Constraints from the Zircon U-Pb Dating and Sr-Nd-Pb-Hf Isotopic Systematics. Earth Science, 34(1): 1-10.

    The Petrogenesis of Late Mesozoic Volcanic Rock and the Contributions from Ancient Micro-Continents: Constraints from the Zircon U-Pb Dating and Sr-Nd-Pb-Hf Isotopic Systematics

    • Received Date: 2008-12-01
    • Publish Date: 2009-01-25
    • Comprehensive geochemical investigations on the Late Mesozoic volcanic rocks from Tahe and Xiwu areas, Great Xing'an range reveal that the mantle sources for these rocks are of attributes of old continent blocks, while the mantle sources for the coeval volcanic rocks from other area show juvenile features.The detrital zircons from Tahe volcanic rocks have records of Late Proterozoic and Early Paleozoic.Trace elements and Sr, Nd, Pb and Hf isotopic features imply that the mantle sources for these two volcanic fields were inherited from enriched lithospheric mantle beneath old blocks with overprint of subducted juvenile island arc materials.This study provides solid deep geochemical constraints on the existence of Precambrian blocks among the Paleozoic Xingmeng orogen.During the Late Mesozoic, with the closure of the Mongol-Okhotsk and Mesozoic global event, regional extensional geological setting developed in these regions, which trigged decompressional melting of the lithospheric mantle and caused the voluminous eruption of volcanic rocks.

       

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