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• W2336692996 abstract "Small irregular to lens-like occurrences (maximum 0.5 × 1 m) of apatite associated with magnetite and silicates are present in the Agoriani area of the Othrys ophiolite complex, central Greece. The Ano Agoriani area is dominated by peridotite (plagioclase lherzolite) of the mantle sequence, intruded by irregular bodies, dikes, and veins of gabbro, as well as by dikes of pyroxenite and pegmatitic gabbro. Apatite occurs as large (up to 3 cm long) well-formed crystals associated with magnetite. The aggregates consist predominantly of apatite, or massive magnetite with subordinate amounts of apatite." @default.
• W2336692996 created "2016-06-24" @default.
• W2336692996 creator A5012166738 @default.
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• W2336692996 date "2001-10-01" @default.
• W2336692996 modified "2023-10-16" @default.
• W2336692996 title "Occurrence of apatite associated with magnetite in an ophiolite complex (Othrys), Greece" @default.
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• W2336692996 doi "https://doi.org/10.2138/am-2001-1003" @default.
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