Mesozoic crust-mantle interaction beneath the North China craton: A consequence of the dispersal of Gondwanaland and accretion of Asia

Geology - Tập 31 Số 9 - Trang 817 - 2003
Simon A. Wilde1, Xinhua Zhou2, A. A. Nemchin3, Min Sun4
1Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia
2Department of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing, China
3Department of Mining and Exploration Geology, West Australian School of Mines, Curtin University of Technology, Kalgoorlie, WA 6433, Australia
4Department of Earth Sciences, University of Hong Kong, Pokfulum Road, Hong Kong, China

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