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Skip to Search Results- 1Carvalho, Luísa D.V.
- 1Czas, Janina
- 1Fuck, Reinhardt A.
- 1Gonçalves, Guilherme O.
- 1Jalowitzki, Tiago
- 1Pearson, D. Graham
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Age, origin and composition of the Attawapiskat lithospheric mantle and its diamonds (western Superior craton, Canada)
DownloadFall 2013
This study reports results from peridotitic and eclogitic xenoliths and di- amond samples from the Attawapiskat area to understand the processes of craton formation and modification in the Superior lithospheric mantle. These diamondiferous kimberlites also provide an opportunity to study the...
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Diamond formation beneath the Coromandel area, southwestern São Francisco Craton – The role of re-fertilization and subduction
Download2022-01-01
Carvalho, Luísa D.V., Stachel, Thomas, Pearson, D. Graham, Fuck, Reinhardt A., Jalowitzki, Tiago, Timmerman, Suzette, Steele-Maclnnis, Matthew, Gonçalves, Guilherme O., Pereira, Rogério Silvestre, Scholz, Ricardo
Abstract The lithospheric mantle underpinning the Alto Paranaíba Igneous Province, southwestern São Francisco Craton, was investigated through a study of 82 diamonds and their mineral inclusions from the Coromandel (Douradinho River), Verde River (northern Coromandel), Abaeté, Frutal, and Romaria...
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The Quandary of the Sask Craton: Origin and Evolution of the Lithospheric Mantle beneath the Sask Craton
DownloadFall 2018
Mantle xenoliths from the Cretaceous (~106 to ~95 Ma) kimberlites at Fort à la Corne (FALC) present a unique opportunity to study the lithospheric mantle beneath the newly recognised Sask Craton. The Sask Craton, a small terrane with Archean (3.2 - 2.5 Ga) crustal ages, is enclosed in the...