Reply

Publisher's version (útgefin grein) 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...

Full description

Bibliographic Details
Main Authors: Bjarnason, Ingi Þorleifur, Menke, William, Flóvenz, Ólafur G.
Other Authors: Jarðvísindastofnun (HÍ), Institute of Earth Sciences (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 1994
Subjects:
Jarðeðlisfræði
Jarðmöttull
Jarðskorpa
Jarðhiti
Iceland
Online Access:https://hdl.handle.net/20.500.11815/1234
id ftopinvisindi:oai:opinvisindi.is:20.500.11815/1234
record_format openpolar
spelling ftopinvisindi:oai:opinvisindi.is:20.500.11815/1234 2023-05-15T16:47:19+02:00 Reply Bjarnason, Ingi Þorleifur Menke, William Flóvenz, Ólafur G. Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 1994-09-10 17,915-17,917 https://hdl.handle.net/20.500.11815/1234 en eng American Geophysical Union Journal of geophysical research;99(B9) 0148-0227 https://hdl.handle.net/20.500.11815/1234 Journal of geophysical research info:eu-repo/semantics/openAccess Jarðeðlisfræði Jarðmöttull Jarðskorpa Jarðhiti info:eu-repo/semantics/article 1994 ftopinvisindi https://doi.org/20.500.11815/1234 2022-11-18T06:51:46Z Publisher's version (útgefin grein) 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. Article in Journal/Newspaper Iceland Opin vísindi (Iceland)
institution Open Polar
collection Opin vísindi (Iceland)
op_collection_id ftopinvisindi
language English
topic Jarðeðlisfræði
Jarðmöttull
Jarðskorpa
Jarðhiti
spellingShingle Jarðeðlisfræði
Jarðmöttull
Jarðskorpa
Jarðhiti
Bjarnason, Ingi Þorleifur
Menke, William
Flóvenz, Ólafur G.
Reply
topic_facet Jarðeðlisfræði
Jarðmöttull
Jarðskorpa
Jarðhiti
description Publisher's version (útgefin grein) 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.
author2 Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Háskóli Íslands
University of Iceland
format Article in Journal/Newspaper
author Bjarnason, Ingi Þorleifur
Menke, William
Flóvenz, Ólafur G.
author_facet Bjarnason, Ingi Þorleifur
Menke, William
Flóvenz, Ólafur G.
author_sort Bjarnason, Ingi Þorleifur
title Reply
title_short Reply
title_full Reply
title_fullStr Reply
title_full_unstemmed Reply
title_sort reply
publisher American Geophysical Union
publishDate 1994
url https://hdl.handle.net/20.500.11815/1234
genre Iceland
genre_facet Iceland
op_relation Journal of geophysical research;99(B9)
0148-0227
https://hdl.handle.net/20.500.11815/1234
Journal of geophysical research
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/20.500.11815/1234
_version_ 1766037410530983936

Similar Items