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)

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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...

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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

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