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- W2024776908 abstract "Mantle peridotite (lherzolite) is one of the most important rock units of the Jandaq ophiolite (central Iran). This ophiolite suffered numerous phases of metamorphism, and is covered by Paleozoic schist and marble metamorphic rocks. Metamorphic minerals found are olivine, tremolite, orthopyroxene, talc, anthophyllite, chlorite, serpentine and magnetite. Clinopyroxene and chromian spinel, the most resistant minerals against metamorphism and alteration, are relicts of the primary igneous mineralogy. One of the most important characteristics of the mantle peridotites in Jandaq ophiolites is the absence of chromitite, due to the low Cr- and high Al-nature of these mantle rocks, as well as non-extensive mantle partial melting during continual production of ascending melt. The Jandaq peridotite belongs to the LOT-type, and has no chromitite potential. Une péridotite mantellique lherzolitique est l’un des types pétrographiques principaux constituant l’ophiolite de Jandaq (Iran central). Recouverte de marbres et schistes paléozoïquues, cette ophiolite a subi de nombreuses phases de métamorphisme. Les minéraux métamorphiques sont olivine, trémolite, orthopyroxène, talc, antophyllite, chlorite, serpentine et magnétite. Clinopyroxènene et spinelle chromifère, plus résistants au métamorphisme et à l’altération, sont des reliques de la minéralogie ignée primaire. L’une des caractéristiques les plus importantes de l’ophiolite de Jandaq est l’absence de chromitites, liée au caractère pauvre en chrome et riche en aluminium de ces roches mantelliques, ainsi qu’à la fusion partielle limitée du manteau durant une production continue de laves ascendantes. De type LOT, la péridotite de Jandaq n’a ainsi aucun potentiel chromifère." @default.
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- W2024776908 date "2009-12-01" @default.
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- W2024776908 title "Chromitite potential in mantle peridotites of the Jandaq ophiolite (central Iran)" @default.
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- W2024776908 doi "https://doi.org/10.1016/j.crte.2009.07.014" @default.
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