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The North China Craton is a classic case for the destruction of an ancient craton, in that it records the loss of more than 100km of ancient refractory lithospheric mantle during the late Mesozoic and early Cenozoic. However, the mechanisms for this lithospheric thinning remain controversial in large part due to the lack of any systematic investigations of the Mesozoic asthenospheric mantle via its...
The Mesozoic granitoids at the southern margin of the North China Craton are of considerable geologic interest, because of their geodynamic context and likely relationship to Mesozoic lithospheric delamination, but also because they are associated with one of the most important gold belts in China. However, their detailed age relations and petrogeneses have not been described by systematic and comprehensive...
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