The high arctic LIP in Canada: Trace element and sm–nd isotopic evidence for the role of mantle heterogeneity and crustal assimilation

The Cretaceous geological evolution of the Canadian Arctic was marked by voluminous magmatism comprising Canada’s portion of the High Arctic large igneous province (HALIP) that is thought to have resulted from a mantle plume head. This magmatism is largely recorded as extensive Early Cretaceous lava...

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Bibliographic Details
Published in:Norwegian Journal of Geology
Main Authors: Kingsbury, C.G. (Cole G.), Ernst, R.E. (Richard E.), Cousens, B. (Brian), Williamson, M.-C. (Marie-Claude)
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://ir.library.carleton.ca/pub/12884
https://doi.org/10.17850/njg96-2-02