Maghemite in Icelandic basalts
Curie temperatures indicating non-titaniferous magnetite are common in Icelandic basalts of all ages, especially Tertiary ones. Yet, microprobe analyses of such samples have shown high titanium in the magnetite. To resolve this paradox, and the mechanism at work, the magnetic mineral fraction of eig...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.606.7801 2023-05-15T16:50:05+02:00 Maghemite in Icelandic basalts S. Steinthorsson Helgason M. B. Madsen C. Bender Koch M. D. Bentzon S. Morup The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.606.7801 http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.606.7801 http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf maghemite basalts M6ssbauer spectroscopy X-ray diffraction Iceland text ftciteseerx 2016-01-08T14:17:42Z Curie temperatures indicating non-titaniferous magnetite are common in Icelandic basalts of all ages, especially Tertiary ones. Yet, microprobe analyses of such samples have shown high titanium in the magnetite. To resolve this paradox, and the mechanism at work, the magnetic mineral fraction of eight basalt samples with J~-T curves characteristic for pure magnetite was subjected to a multi-disciplinary analysis including M6ssbauer spectroscopy and X-ray diffraction. In most of the samples titanium in the magnetite, as analysed with the microprobe, ranged between 16 and 28 wt.%, indicating sub-microscopic solvus exsolution in the titanomagnetite, beyond the power of resolution for the microprobe. More unexpectedly in view of the reversible Js-T curves, MOssbauer spectroscopy showed appreciable proportion of maghemite in the magnetic fraction. A three-stage mechanism is proposed for the formation of the mineral assemblages observed: (1) limited high-temperature oxyexsolution; (2) solvus exsolution during low-temperature hydrothermal teration; and (3) maghemitization f the magnetite. Finally, the maghemite may transform to hematite with time. It is concluded that maghemite is much more common in Icelandic rocks than hitherto believed. Text Iceland Unknown |
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English |
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maghemite basalts M6ssbauer spectroscopy X-ray diffraction Iceland |
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maghemite basalts M6ssbauer spectroscopy X-ray diffraction Iceland S. Steinthorsson Helgason M. B. Madsen C. Bender Koch M. D. Bentzon S. Morup Maghemite in Icelandic basalts |
topic_facet |
maghemite basalts M6ssbauer spectroscopy X-ray diffraction Iceland |
description |
Curie temperatures indicating non-titaniferous magnetite are common in Icelandic basalts of all ages, especially Tertiary ones. Yet, microprobe analyses of such samples have shown high titanium in the magnetite. To resolve this paradox, and the mechanism at work, the magnetic mineral fraction of eight basalt samples with J~-T curves characteristic for pure magnetite was subjected to a multi-disciplinary analysis including M6ssbauer spectroscopy and X-ray diffraction. In most of the samples titanium in the magnetite, as analysed with the microprobe, ranged between 16 and 28 wt.%, indicating sub-microscopic solvus exsolution in the titanomagnetite, beyond the power of resolution for the microprobe. More unexpectedly in view of the reversible Js-T curves, MOssbauer spectroscopy showed appreciable proportion of maghemite in the magnetic fraction. A three-stage mechanism is proposed for the formation of the mineral assemblages observed: (1) limited high-temperature oxyexsolution; (2) solvus exsolution during low-temperature hydrothermal teration; and (3) maghemitization f the magnetite. Finally, the maghemite may transform to hematite with time. It is concluded that maghemite is much more common in Icelandic rocks than hitherto believed. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
S. Steinthorsson Helgason M. B. Madsen C. Bender Koch M. D. Bentzon S. Morup |
author_facet |
S. Steinthorsson Helgason M. B. Madsen C. Bender Koch M. D. Bentzon S. Morup |
author_sort |
S. Steinthorsson |
title |
Maghemite in Icelandic basalts |
title_short |
Maghemite in Icelandic basalts |
title_full |
Maghemite in Icelandic basalts |
title_fullStr |
Maghemite in Icelandic basalts |
title_full_unstemmed |
Maghemite in Icelandic basalts |
title_sort |
maghemite in icelandic basalts |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.606.7801 http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf |
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Iceland |
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Iceland |
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http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.606.7801 http://www.minersoc.org/pages/Archive-MM/Volume_56/56-383-185.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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