Downward rejuvenation of the continental lower crust beneath the southeastern North China Craton

Felsic to mafic granulite xenoliths and zircon xenocrysts from the Cenozoic (~1 Ma) Nushan basalts were analyzed to construct a lower-crustal column illustrating the fine structure and evolution of the deep crust beneath the southeastern North China Craton. Felsic granulites, sampled from the lowerm...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Tectonophysics 2019-01, Vol.750, p.213-228
Hauptverfasser:	Ping, Xianquan, Zheng, Jianping, Xiong, Qing, Griffin, W.L., Yu, Chunmei, Su, Yuping
Format:	Artikel
Sprache:	eng
Schlagworte:	Accretion Age Basalt Cenozoic Columnar structure Continental lower crust Cratons Deposition Downward rejuvenation Evolution Fine structure Granulite xenolith Hafnium isotopes Hf isotopes Isotopes Magma Mesozoic Paleozoic Ratios Recrystallization Southeastern North China Craton Subduction U-Pb ages Ultrastructure Zircon
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!