Volume 26 Issue 5
Oct.  2020
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Article Navigation >  Journal of Geomechanics  > 2020  >  26(5): 742-758
ZHENG Jianping, 2020. Internal and external factors in continental lithosphere mantle replacement in eastern China. Journal of Geomechanics, 26 (5): 742-758. DOI: 10.12090/j.issn.1006-6616.2020.26.05.061
Citation: ZHENG Jianping, 2020. Internal and external factors in continental lithosphere mantle replacement in eastern China. Journal of Geomechanics, 26 (5): 742-758. DOI: 10.12090/j.issn.1006-6616.2020.26.05.061
shu

Internal and external factors in continental lithosphere mantle replacement in eastern China

doi: 10.12090/j.issn.1006-6616.2020.26.05.061
  • 1.

    School of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

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

More Information
  • Received: 2020-07-26
  • Revised: 2020-08-18
  • Published: 2020-10-01
    Abstract
  • Cratonic continent usually has an ancient, thick and refractory lithosphere mantle. Depleted basaltic composition, low density and high rigidity make the cratonic lithosphere float above the asthenosphere enclosure and exist stably for a long time. The eastern China continent was formed through the collision of the North and South China blocks along the Qinling-Dabie-Sulu Orogenic Belt during the Paleozoic and the early Mesozoic, and was reactive in the Phanerozoic, especially in the late Mesozoic. Since then, the eastern China continent showed the charateristics of strong tectonic deformation, basin formation, magmatism and massive mineralization. What are the deep reasons which caused these effects? Based on the analysis of formation and evolution of the eastern continent and the properties of the lithosphere mantle, it can be found that the initial scale of the block was small, and the developed zones were weak and easily affected by later transformation. Especially since the Phanerozoic, the Chinese mainland has been clamped by several surrounding tectonic domains, and the asthenospheric upwellings caused by subductions in different stages and directions have eroded along the weak zones and reformed the overlying lithosphere. These effects led to the thinning lithosphere, significant re-enrichment and ultimate mantle replacement. After the transformation and replacement, the lithosphere mantle that was enriched in basaltic components and had high density and low rigidity, was prone to deformation and partial melting, which made the stable cratonic continent activated. The block scale, internal weak zones and surrounding tectonic environment are, therefore, important internal and external factors in controlling continental stability. The lithospheric evolution of eastern China in the Phanerozoic reflects comprehensive records of these favorable factors.

     

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