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- W1980958034 abstract "The chemical composition of minerals from a suite of Variscan lamprophyres (kersantite, minette, spessartite and vogesite) from the Saxothuringian Zone of the Variscan orogen, Germany, were investigated by electron microprobe. These lamprophyres usually contain small grains (<50 μm) of Zr-bearing titanite as the only primary mineral containing traceable zirconium. A late-stage residual alkaline melt within the lamprophyric magma is considered to have crystallized the Zr-rich titanite. The titanite typically has euhedral Zr-rich cores, mantled by Zr-poor overgrowths. This compositional change is explained by rapid decrease of temperature during magma uprise and emplacement. Relatively high Zr contents and compositional and textural heterogeneities (e.g. syenitic schlieren, veins and globules) within the lamprophyric host rocks are evidence of magma mixing. Incorporation of Zr into titanite apparently takes place as a coupled substitution (Ti4++Al3+⇔Zr4++Fe3+) rather than as a simple 1:1 replacement of Ti by Zr. A ZrO2 content of about 6 wt.% (equivalent to ∼0.10 atoms per formula unit Zr) is implied as the upper concentration limit in titanite. Locally occurring higher values are attributed to tiny inclusions of secondary Zr phases. In carbonate-rich portions of lamprophyres, titanite is transformed into an unindentified TiO2 phase. High-(Al,F) titanite (XAl up to 0.54), restricted in occurrence to the contact between tonalite porphyry and kersantite, formed under the conditions of high fluorine activity connected with the rhyolitic magmatism. The results show that the Zr budget of lamprophyres, and possibly of other mafic igneous rocks lacking zircon, is strongly governed by titanite. Element distribution patterns in titanite are a key to the better understanding of magmatic evolution and petrogenesis of lamprophyres." @default.
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- W1980958034 date "2003-11-01" @default.
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- W1980958034 title "Accessory titanite: an important carrier of zirconium in lamprophyres" @default.
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- W1980958034 doi "https://doi.org/10.1016/j.lithos.2003.07.002" @default.
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