Autor:	A L, Perchuk, T V, Gerya, V S, Zakharov, W L, Griffin
Rok vydání:	2019
Zdroj:	Nature. 586(7829)
ISSN:	1476-4687
Popis:	The ancient cores of continents (cratons) are underlain by mantle keels-volumes of melt-depleted, mechanically resistant, buoyant and diamondiferous mantle up to 350 kilometres thick, which have remained isolated from the hotter and denser convecting mantle for more than two billion years. Mantle keels formed only in the Early Earth (approximately 1.5 to 3.5 billion years ago in the Precambrian eon); they have no modern analogues
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=pmid________::d1d867d54004fe34fb3d7ed06e57c507 https://pubmed.ncbi.nlm.nih.gov/33057224 Zobrazit plný text záznamu Full text from SpringerLink