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Lenaz, Davide, Adetunji, Jacob, Rollinson, Hugh (2014) Determination of Fe3+/ΣFe ratios in chrome spinels using a combined Mössbauer and single-crystal X-ray approach: application to chromitites from the mantle section of the Oman ophiolite. Contributions to Mineralogy and Petrology, 167 (1) doi:10.1007/s00410-013-0958-2

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Reference TypeJournal (article/letter/editorial)
TitleDetermination of Fe3+/ΣFe ratios in chrome spinels using a combined Mössbauer and single-crystal X-ray approach: application to chromitites from the mantle section of the Oman ophiolite
JournalContributions to Mineralogy and Petrology
AuthorsLenaz, DavideAuthor
Adetunji, JacobAuthor
Rollinson, HughAuthor
Year2014 (January)Volume167
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-013-0958-2Search in ResearchGate
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Mindat Ref. ID79587Long-form Identifiermindat:1:5:79587:4
GUID0
Full ReferenceLenaz, Davide, Adetunji, Jacob, Rollinson, Hugh (2014) Determination of Fe3+/ΣFe ratios in chrome spinels using a combined Mössbauer and single-crystal X-ray approach: application to chromitites from the mantle section of the Oman ophiolite. Contributions to Mineralogy and Petrology, 167 (1) doi:10.1007/s00410-013-0958-2
Plain TextLenaz, Davide, Adetunji, Jacob, Rollinson, Hugh (2014) Determination of Fe3+/ΣFe ratios in chrome spinels using a combined Mössbauer and single-crystal X-ray approach: application to chromitites from the mantle section of the Oman ophiolite. Contributions to Mineralogy and Petrology, 167 (1) doi:10.1007/s00410-013-0958-2
In(2014, January) Contributions to Mineralogy and Petrology Vol. 167 (1) Springer Science and Business Media LLC

See Also

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Rollinson, Hugh, Adetunji, Jacob, Lenaz, Davide, Szilas, Kristoffer (2017) Archaean chromitites show constant Fe3+/ΣFe in Earth's asthenospheric mantle since 3.8 Ga. Lithos, 282. 316-325 doi:10.1016/j.lithos.2017.03.020
Rollinson, Hugh (2008) The geochemistry of mantle chromitites from the northern part of the Oman ophiolite: inferred parental melt compositions. Contributions to Mineralogy and Petrology, 156 (3) 273-288 doi:10.1007/s00410-008-0284-2
Rollinson, Hugh (2015) Slab and sediment melting during subduction initiation: granitoid dykes from the mantle section of the Oman ophiolite. Contributions to Mineralogy and Petrology, 170 (3) doi:10.1007/s00410-015-1177-9
Rollinson, Hugh, Adetunji, Jacob (2015) The geochemistry and oxidation state of podiform chromitites from the mantle section of the Oman ophiolite: A review. Gondwana Research, 27 (2) 543-554 doi:10.1016/j.gr.2013.07.013
Rollinson, H., Adetunji, J., Yousif, A. A., Gismelseed, A. M. (2012) New Mössbauer measurements of Fe3+/ΣFe in chromites from the mantle section of the Oman ophiolite: evidence for the oxidation of the sub-oceanic mantle. Mineralogical Magazine, 76 (3) 579-596 doi:10.1180/minmag.2012.076.3.09
Adetunji, Jacob, Everitt, Simon, Rollinson, Hugh (2013) New Mössbauer measurements of Fe3+/ΣFe ratios in chromites from the early Proterozoic Bushveld Complex, South Africa. Precambrian Research, 228. 194-205 doi:10.1016/j.precamres.2013.01.007
Rollinson, Hugh, Adetunji, Jacob (2013) Mantle podiform chromitites do not form beneath mid-ocean ridges: A case study from the Moho transition zone of the Oman ophiolite. Lithos, 177. 314-327 doi:10.1016/j.lithos.2013.07.004
ROLLINSON, Hugh, ADETUNJI, Jacob (2015) Chromite in the Mantle Section of the Oman Ophiolite: Implications for the Tectonic Evolution of the Oman Ophiolite. Acta Geologica Sinica - English Edition, 89. 73-76 doi:10.1111/1755-6724.12308_44
Rollinson, Hugh (2007) Recognising early Archaean mantle: a reappraisal. Contributions to Mineralogy and Petrology, 154 (3) 241-252 doi:10.1007/s00410-007-0191-y
Ahmed, A., Arai, S. (2002) Unexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonic implications. Contributions to Mineralogy and Petrology, 143 (3) 263-278 doi:10.1007/s00410-002-0347-8
Rollinson, Hugh (2023) The growth of the Zimbabwe craton during the Neoarchaean. Contributions to Mineralogy and Petrology, 178 (1) doi:10.1007/s00410-022-01978-7
 
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