Zircon U–Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic
about
Zircon U–Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic
description
article
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2008
@uk
name
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@en
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@nl
type
label
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@en
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@nl
prefLabel
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@en
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@nl
P2093
P50
P1433
P1476
Zircon U–Pb and Hf isotopic st ...... the early to middle Palaeozoic
@en
P2093
P304
P356
10.1016/J.CHEMGEO.2007.10.026
P577
2008-01-01T00:00:00Z