Paleozoic adakitic rocks in the northern Altyn Tagh, northwest China: Evidence for progressive crustal thickening beneath the Dunhuang Block
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文摘
Three Late Paleozoic adakitic intrusions are discovered in the Dunhuang Block. The rocks were generated by partial melting of a thickened lower crus. The crustal thickening started prior to the Middle Devonian and lasted more than 50 Ma. The crustal thickness in the Early Carboniferous is thicker than that in the Late Devonian.
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