A chemical Earth model with whole mantle convection: the importance of a core-mantle boundary layer (D ) and its early formation

Tolstikhin, Igor; Kramers, Jan Dirk; Hofmann, A (2006). A chemical Earth model with whole mantle convection: the importance of a core-mantle boundary layer (D ) and its early formation. Chemical geology, 226(3-4), pp. 79-99. Amsterdam: Elsevier 10.1016/j.chemgeo.2005.09.015

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Item Type:	Journal Article (Original Article)
Division/Institute:	08 Faculty of Science > Institute of Geological Sciences
UniBE Contributor:	Kramers, Jan Dirk
ISSN:	0009-2541
Publisher:	Elsevier
Language:	English
Submitter:	Factscience Import
Date Deposited:	04 Oct 2013 15:00
Last Modified:	05 Dec 2022 14:18
Publisher DOI:	10.1016/j.chemgeo.2005.09.015
Web of Science ID:	000235857100002
URI:	https://boris.unibe.ch/id/eprint/25990 (FactScience: 62718)