Age and provenance constraints on seismically-determined crustal layers beneath the Paleozoic southern Central Asian Orogen, Inner Mongolia, China
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文摘

Zircon ages explain the crustal composition of a seismic transect across Inner Mongolia.

The middle crust comprises Proterozoic mafic and felsic gneisses.

The lower crust forms a late Archaean granulite-facies assemblage.

The deep crust of the southern CAOB and the northern NCC have a similar provenance.

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