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- W2084815572 abstract "The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism." @default.
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- W2084815572 date "2003-03-01" @default.
- W2084815572 modified "2023-09-25" @default.
- W2084815572 title "The lamprophyres of Afyon stratovolcano, western Anatolia, Turkey: description and genesis" @default.
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- W2084815572 doi "https://doi.org/10.1016/s1631-0713(03)00049-x" @default.
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