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Ingi Þorleifur Bjarnason; William Menke; Ólafur G. Flóvenz

Reply

Ingi Þorleifur Bjarnason
, William Menke
, Ólafur G. Flóvenz

University of Iceland

Háskóli Íslands

Rannsóknarafurð: Framlag til fræðitímarits › Grein

Útdráttur

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.

Upprunalegt tungumál	Enska
Síður (frá-til)	17,915-17,917
Fræðitímarit	Journal of Geophysical Research
Bindi	99
Númer tölublaðs	B9
Útgáfustaða	Útgefið - 10 sep. 1994

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https://hdl.handle.net/20.500.11815/1234

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AU - Bjarnason, Ingi Þorleifur

AU - Menke, William

AU - Flóvenz, Ólafur G.

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N2 - 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.

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KW - Jarðeðlisfræði

KW - Jarðhiti

KW - Jarðmöttull

KW - Jarðskorpa

KW - Jarðeðlisfræði

KW - Jarðhiti

KW - Jarðmöttull

KW - Jarðskorpa

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