Heat Generation in Cratonic Mantle Roots—New Trace Element Constraints From Mantle Xenoliths and Implications for Cratonic Geotherms-Reference-Cited by-同舟云学术

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Heat Generation in Cratonic Mantle Roots—New Trace Element Constraints From Mantle Xenoliths and Implications for Cratonic Geotherms

Published:2021-09 Issue:9 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

McIntyre T.¹^ORCID,Kublik K.¹^ORCID,Currie C.¹^ORCID,Pearson D. G.¹^ORCID

Affiliation:

1. Department of Earth & Atmospheric Sciences University of Alberta Edmonton AB Canada

Funder

Canada Excellence Research Chairs, Government of Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009691

Reference109 articles.

1. Metasomatism in lithospheric mantle roots: Constraints from whole-rock and mineral chemical composition of deformed peridotite xenoliths from kimberlite pipe Udachnaya

2. Persistence of fertile and hydrous lithospheric mantle beneath the northwestern Ethiopian plateau: Evidence from modal, trace element and Sr–Nd–Hf isotopic compositions of amphibole-bearing mantle xenoliths

3. Lithosphere thermal thickness and geothermal heat flux in Greenland from a new thermal isostasy method

4. Major- and trace-elements in cratonic mantle eclogites and pyroxenites reveal heterogeneous sources and metamorphic processing of low-pressure protoliths

5. Origins of cratonic mantle discontinuities: A view from petrology, geochemistry and thermodynamic models

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