Thermochemical structure of the Superior craton and environs: Implications for the evolution and preservation of cratonic lithosphere
The Archean Superior craton was formed by the assemblage of continental and oceanic terranes at ∼2.6 Ga. The craton is surrounded by multiple Proterozoic mobile belts, including the Paleoproterozoic Trans-Hudson Orogen which brought together the Superior and Rae/Hearne cratons at ∼1.9-1.8 Ga. Despit...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | unknown |
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Authorea, Inc.
2024
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Subjects: | |
Online Access: | http://dx.doi.org/10.22541/essoar.170612483.37231728/v1 |