Computer Science
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State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 10029, China
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, PR China
Chondritic magnesium isotopic composition of the terrestrial mantle: A case study of peridotite xenoliths from the North China craton
Comments on ``Petrology of the Hegenshan ophiolite and its implication for the tectonic evolution of northern China'' by T. Nozaka and Y. Liu [Earth Planet. Sci. Lett. 202 (2002) 89-104]
Highly heterogeneous Mesozoic lithospheric mantle beneath the North China Craton: Evidence from Sr-Nd-Pb isotopic systematics of mafic rocks
Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt rock interaction in the considerably thinned lithospheric mantle
Re-Os isotopic variation in melt/rock interaction: Implication for the Re-Os age of lithospheric mantle beneath the North China craton
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