Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic

Article

Abstract: Gneissic rocks in the Chinese Altai Mountains have been interpreted as either Paleozoic metasediment

Palabras claves:

Altaids, Gneiss, Hf isotope, U-Pb age, zircon

Autores:

Alfred Kron̈er, Lin S., Long X., Sun M., Wu F.Y., Xia X., Xiao W., Yuan C., Zhao G.C.

Fuentes:

scopus