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Lithospheric thinning and destruction of the North China Craton.

WU FuYuan~1 XU YiGang~2 GAO Shan~3 ZHENG JianPing~3 1.State Key Laborntory of Lithoshperic Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Key Laboratory of Isotopic Geochronology and Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China 3.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China  
Lithospheric thinning and destruction of the North China Craton are intensively discussed in recent literature.It is unclear,however,about its time,thinning degree,spatial variation,mechanism and tectonic controlling factors for this kind of geodynamic phenomena.A comprehensive review and discussion is given in this paper,including:(1) Difference between lithospheric thinning and cratonic destruction;(2) Lithospheric mantle ages beneath the North China Craton since Paleozoic and crust-mantle decoupling;(3) Time of the lithospheric thinning and destruction;(4) Vertical thining variations in the lithosphere;(5) Spatial variations in whole eastern China;(6) Mechanism;(7) Geodynamic controlling factors;(8) Uniqueness of the destruction of the North China Craton on the Earth.Finally,a compilation of references on the lithospheric thinning and destruction of the North China Craton is given in the appendix.
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