Asthenosphere–lithosphere interaction triggered by a slab window during ridge subduction: Trace element and Sr–Nd–Hf–Os isotopic evidence from Late Carboniferous tholeiites in the western Junggar area (NW China)

Asthenosphere–lithosphere interaction triggered by a slab window during ridge subduction: Trace element and Sr–Nd–Hf–Os isotopic evidence from Late Carboniferous tholeiites in the western Junggar area (NW China)

Tholeiites occur in a variety of geological settings, e.g., mid-ocean ridge, back-arc basin, ocean island, island arc and intra-continent, and their geochemical and isotopic characteristics vary according to the corresponding geodynamic environments. Here we investigated the Hatu tholeiitic basalts...

Full description

Bibliographic Details
Main Authors: Tang, G., Wyman, D., Wang, Q., Li, J., Li, Zheng-Xiang, Zhao, Z., Sun, W.
Format: Journal Article
Published: Elsevier Science BV 2012
Subjects:
ridge subduction
asthenosphere
slab window
tholeiites
Central Asian Orogenic Belt
Online Access:http://hdl.handle.net/20.500.11937/11837

Internet

http://hdl.handle.net/20.500.11937/11837

Similar Items