Reply
| dc.contributor | Háskóli Íslands | en_US |
| dc.contributor | University of Iceland | en_US |
| dc.contributor.author | Bjarnason, Ingi Þorleifur | |
| dc.contributor.author | Menke, William | |
| dc.contributor.author | Flóvenz, Ólafur G. | |
| dc.contributor.department | Jarðvísindastofnun (HÍ) | en_US |
| dc.contributor.department | Institute of Earth Sciences (UI) | en_US |
| dc.contributor.school | Verkfræði- og náttúruvísindasvið (HÍ) | en_US |
| dc.contributor.school | School of Engineering and Natural Sciences (UI) | en_US |
| dc.date.accessioned | 2019-09-02T14:40:59Z | |
| dc.date.available | 2019-09-02T14:40:59Z | |
| dc.date.issued | 1994-09-10 | |
| dc.description | Publisher's version (útgefin grein) | en_US |
| 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. | is |
| dc.format.extent | 17,915-17,917 | is |
| dc.identifier.issn | 0148-0227 | |
| dc.identifier.journal | Journal of geophysical research | en_US |
| dc.identifier.uri | https://hdl.handle.net/20.500.11815/1234 | |
| dc.language.iso | en | en_US |
| dc.publisher | American Geophysical Union | en_US |
| dc.relation.ispartofseries | Journal of geophysical research;99(B9) | |
| dc.rights | info:eu-repo/semantics/openAccess | en_US |
| dc.subject | Jarðeðlisfræði | en_US |
| dc.subject | Jarðmöttull | en_US |
| dc.subject | Jarðskorpa | en_US |
| dc.subject | Jarðhiti | en_US |
| dc.title | Reply | en_US |
| dc.type | info:eu-repo/semantics/article | en_US |
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