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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...
| Main Authors: | , , |
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| Other Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
American Geophysical Union
1994
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| Subjects: | |
| Online Access: | https://hdl.handle.net/20.500.11815/1234 |
| _version_ | 1835016291582214144 |
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| author | Bjarnason, Ingi Þorleifur Menke, William Flóvenz, Ólafur G. |
| author2 | Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland |
| author_facet | Bjarnason, Ingi Þorleifur Menke, William Flóvenz, Ólafur G. |
| author_sort | Bjarnason, Ingi Þorleifur |
| collection | Unknown |
| 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. |
| format | Article in Journal/Newspaper |
| genre | Iceland |
| genre_facet | Iceland |
| id | ftopinvisindi:oai:opinvisindi.is:20.500.11815/1234 |
| institution | Open Polar |
| language | English |
| op_collection_id | ftopinvisindi |
| op_doi | https://doi.org/20.500.11815/1234 |
| op_relation | Journal of geophysical research;99(B9) https://hdl.handle.net/20.500.11815/1234 Journal of geophysical research |
| op_rights | info:eu-repo/semantics/openAccess |
| publishDate | 1994 |
| publisher | American Geophysical Union |
| record_format | openpolar |
| spelling | ftopinvisindi:oai:opinvisindi.is:20.500.11815/1234 2025-06-15T14:30:11+00:00 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) 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 2025-05-23T03:05:41Z 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 Unknown |
| spellingShingle | Jarðeðlisfræði Jarðmöttull Jarðskorpa Jarðhiti Bjarnason, Ingi Þorleifur Menke, William Flóvenz, Ólafur G. Reply |
| title | Reply |
| title_full | Reply |
| title_fullStr | Reply |
| title_full_unstemmed | Reply |
| title_short | Reply |
| title_sort | reply |
| topic | Jarðeðlisfræði Jarðmöttull Jarðskorpa Jarðhiti |
| topic_facet | Jarðeðlisfræði Jarðmöttull Jarðskorpa Jarðhiti |
| url | https://hdl.handle.net/20.500.11815/1234 |