The Paleoproterozoic Otish Gabbro suite and coeval dyke swarms of the Superior Province: Probing the ca. 2.17 Ga mantle
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference103 articles.
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3. Partitioning coefficients between olivine and silicate melts;Bédard;Lithos,2005
4. Basin evolution and unconformity-related uranium mineralization: the Camie River U prospect, Paleoproterozoic Otish Basin, Quebec;Beyer;Econ. Geol.,2012
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1. The Corrugated Hills Continental Flood Basalt: a c. 2.17 Ga flood basalt province related to breakup of the Superior craton;Geological Society, London, Special Publications;2023-10-24
2. Geochronology and chemostratigraphy of the 2.47–1.96 Ga rift-related volcano-sedimentary succession in the Karasjok Greenstone Belt, northern Norway, and its regional correlation within the Fennoscandian Shield;Precambrian Research;2023-10
3. Uranium mobility and deposition over 1.3 Ga in the Westmoreland area (McArthur Basin, Australia);Mineralium Deposita;2021-01-05
4. Roberts Lake Syncline mafic lavas (NE Superior craton): A proposed extension of the Cape Smith belt;Lithos;2020-08
5. Pb-Pb baddeleyite ages of mafic dykes from the Western Dharwar Craton, Southern India: a window into 2.21–2.18 Ga global mafic magmatism;Journal of Asian Earth Sciences;2020-04
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