中生代华北南缘带状岩石圈结构特征及其大陆形成演化意义

郑建平; 余淳梅; 苏玉平; 汤华云; 魏启荣; 张志海; 路凤香

Volume 34 Issue 1

Jan. 2009

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Article Navigation > Earth Science > 2009 > 34(1): 28-36

ZHENG Jian-ping, YU Chun-mei, SU Yu-ping, TANG Hua-yun, WEI Qi-rong, ZHANG Zhi-hai, LU Feng-xiang, 2009. Mesozoic Zonal Lithosphere beneath the Southern Margin of the North China: Significance for Continental Formation and Evolution. Earth Science, 34(1): 28-36.

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Mesozoic Zonal Lithosphere beneath the Southern Margin of the North China: Significance for Continental Formation and Evolution

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2008-11-01
Publish Date: 2009-01-25

Abstract

Abstract

The formation and destruction of the continental root is one of the most important going topics on the solid earth sciences.A series of deep-seated xenoliths, including mafic to felsic granulite, eclogite, metagabbro, pyroxenite and peridotite, from the Xinyang area with unique temporal and spatial meaning, at southern margin of the North China, were used to dating in ages and properties.The geometrical model of the zonal lithosphere structure in age and composition were suggested for the conjoint position of multi-blocks in Mesozoic (~160Ma).Basing on the zonal lithosphere, the authors also discussed the dynamic processes for its formation.The exposed rocks up to ca.2.85Ga old are underlain by felsic granulites and rare pyroxenites with zircon ages of 3.6-3.4Ga (to ca.30km depth).Deeper (ca.30-45km) parts of the lower crust consist of high-pressure mafic to felsic granulite and meta-gabbro, which give Paleoproterozoic (2.0-1.8Ga) zircon ages.Our data show the significance of underplating and vertical crustal growth in the Paleoproterozoic, which was related to the amalgamation of the eastern and western block of this craton and a global (Columbia) supercontinent assembly.Hf-isotope data indicate that both juvenile material and remelting of older (3.8-3.0Ga) crustal rocks were involved in this important event.Paleozoic (440-260Ma) and Early Mesozoic (228-219Ma) zircons are also found in xenoliths from the deeper part of the lower crust and the uppermost mantle (i.e., eclogite and peridotite).They are interpreted as reflecting geodynamic processes related to the continental collision between this craton and the Yangtze craton, respectively.The xenoliths from Xinyang diatremes thus record the growth and modification of the old (Paleo-Mesoarchean?) continental lithosphere by magma underplating during several tectonic events: assembly of the southern and northern parts of the Eastern Block in Neoarchean time, collision of the western and eastern blocks along the Trans-China orogen in the Paleoproterozoic, and subduction and collision of the Yangtze craton with the North China craton in early Paleozoic and Triassic times, respectively.
- southern margin of the North China,
- Mesozoic,
- zonal lithosphere,
- deep-seated xenolith,
- dynamic mechanism,
- continental formation and evolution,

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Mesozoic Zonal Lithosphere beneath the Southern Margin of the North China: Significance for Continental Formation and Evolution

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