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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

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Reference TypeJournal (article/letter/editorial)
TitleUnexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonic implications
JournalContributions to Mineralogy and Petrology
AuthorsAhmed, A.Author
Arai, S.Author
Year2002 (June)Volume143
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-002-0347-8Search in ResearchGate
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Mindat Ref. ID78140Long-form Identifiermindat:1:5:78140:0
GUID0
Full ReferenceAhmed, 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
Plain TextAhmed, 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
In(2002, June) Contributions to Mineralogy and Petrology Vol. 143 (3) Springer Science and Business Media LLC

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Arai, Shoji, Uesugi, Jiro, Ahmed, Ahmed H. (2004) Upper crustal podiform chromitite from the northern Oman ophiolite as the stratigraphically shallowest chromitite in ophiolite and its implication for Cr concentration. Contributions to Mineralogy and Petrology, 147 (2) 145-154 doi:10.1007/s00410-004-0552-8
Ahmed, A. H., Arai, S., & Kadoshima, K. (2002). Possible platinum-group element (PGE) oxides in the PGE-mineralized chromitite from the Northern Oman Ophiolite. Journal of mineralogical and petrological sciences, 97(4), 190-198.
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 (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
AHMED, Ahmed H., ARAI, Shoji, KADOSHIMA, Kazuyuki (2002) Possible platinum-group element (PGE) oxides in the PGE-mineralized chromitite from the Northern Oman Ophiolite. Journal of Mineralogical and Petrological Sciences, 97 (4) 190-198 doi:10.2465/jmps.97.190
Akizawa, Norikatsu, Arai, Shoji, Tamura, Akihiro (2012) Behavior of MORB magmas at uppermost mantle beneath a fast-spreading axis: an example from Wadi Fizh of the northern Oman ophiolite. Contributions to Mineralogy and Petrology, 164 (4) 601-625 doi:10.1007/s00410-012-0762-4
Schmidt, Gerhard, Snow, Jonathan (2002) Os isotopes in mantle xenoliths from the Eifel volcanic field and the Vogelsberg (Germany): age constraints on the lithospheric mantle. Contributions to Mineralogy and Petrology, 143 (6) 694-705 doi:10.1007/s00410-002-0372-7
Ginibre, Catherine, Wörner, Gerhard, Kronz, Andreas (2002) Minor- and trace-element zoning in plagioclase: implications for magma chamber processes at Parinacota volcano, northern Chile. Contributions to Mineralogy and Petrology, 143 (3) 300-315 doi:10.1007/s00410-002-0351-z
Harris, Chris, Ashwal, Lewis D. (2002) The origin of low δ18O granites and related rocks from the Seychelles. Contributions to Mineralogy and Petrology, 143 (3) 366-376 doi:10.1007/s00410-002-0349-6
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
Wang, Zhihong, Sun, Shu, Li, Jiliang, Hou, Quanlin (2002) Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins. Contributions to Mineralogy and Petrology, 143 (4) 471-483 doi:10.1007/s00410-002-0358-5
 
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