Reply

dc.contributor	Háskóli Íslands
dc.contributor	University of Iceland
dc.contributor.author	orcid.org/0000-0001-5716-7053 Bjarnason, Ingi Þorleifur
dc.contributor.author	Menke, William
dc.contributor.author	Flóvenz, Ólafur G.
dc.date.accessioned	2019-09-02T14:40:59Z
dc.date.available	2019-09-02T14:40:59Z
dc.date.issued	1994-09-10
dc.identifier.issn	0148-0227
dc.identifier.uri	https://hdl.handle.net/20.500.11815/1234
dc.description	Publisher's version (útgefin grein)
dc.description.abstract	The central question discussed by Gudmundsson [this issue] can be succinctly stated: "Is the temperature of the shallowest upper mantle of Iceland at the peridotite solidus" (nominally, 1200°C). The traditional view, as developed by numerous authors during the 1970s and early 1980s (reviewed by Palmason [1986]) and to which Gudmundsson ascribes, is that it is supersolidus and partially molten.
dc.format.extent	17,915-17,917
dc.language.iso	en
dc.publisher	American Geophysical Union
dc.relation.ispartofseries	Journal of geophysical research;99(B9)
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Jarðeðlisfræði
dc.subject	Jarðmöttull
dc.subject	Jarðskorpa
dc.subject	Jarðhiti
dc.title	Reply
dc.type	info:eu-repo/semantics/article
dc.identifier.journal	Journal of geophysical research
dc.contributor.department	Jarðvísindastofnun (HÍ)
dc.contributor.department	Institute of Earth Sciences (UI)
dc.contributor.school	Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school	School of Engineering and Natural Sciences (UI)