The North America mid-Cretaceous kimberlite corridor: Wet, edge-driven decompression melting of an OIB-type deep mantle source
Author:
Affiliation:
1. Geological Survey of Canada; Ottawa Ontario Canada
2. Department of Earth and Atmospheric Sciences; University of Alberta; Edmonton Alberta Canada
Funder
Natural Sciences and Engineering Research Council of Canada
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006761/fullpdf
Reference134 articles.
1. Relationships between mineralogical, chemical and isotopic properties of some North American kimberlites;Alibert;J. Geophys. Res.,1988
2. Age and origin of the Jan Lake Complex: A glimpse at the buried Archean craton of the Trans-Hudson Orogen;Ashton;Can. J. Earth Sci.,1999
3. Two Neoarchean supercontinents? Evidence from the Paleoproterozoic;Aspler;Sediment Geol.,1998
4. The timing of late Cretaceous alkalic igneous activity in the northern Gulf of Mexico;Baksi;J. Geol.,1999
5. Nd and Sr isotopic compositions of East African carbonatites: Implications for mantle heterogeneity;Bell;Geology,1987
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3. Early Eocene Arctic volcanism from carbonate-metasomatized mantle;Contributions to Mineralogy and Petrology;2023-11-20
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