Mineralogy and petrology of leucite ankaratrites with affinities to kamafugites and carbonatites from the Kayıköy area, Isparta, SW Anatolia, Turkey: Implications for the influences of carbonatite metasomatism into the parental mantle sources of silica-undersaturated potassic magmas
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- 作者：Şemsettin Caran ; semsettincaran@sdu.edu.tr" class="auth_mail" title="E-mail the corresponding author
- 关键词：Leucite ankaratrite ; Kamafugitic affinity ; Carbonatite infiltration ; Isparta ; Kayıkö ; y ; SW Turkey
- 刊名：Lithos
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：256-257
- 期：Complete
- 页码：13-25
- 全文大小：3319 K
文摘
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The range of coeval potassic magmatism in the Isparta Angle, SW Turkey is a natural laboratory to elucidate the mantle beneath the region.
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The Kayıköy leucite-ankaratrites represent most silica-deficient mafic potassic lavas within the Inner Isparta Angle volcanic province.
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The major, trace element and isotope compositions of the Kayıköy leucite-ankaratrites show affinities to kamafugites and carbonatites.
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Mixing of both carbonate and silicate melts from asthenosphere produced carbonated phonolitic melts.
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The carbonate-bearing phonolitic melts react with peridotitic wall rock to produce wherlitic metasomes.
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The leucite-ankaratrites are derived from partial melting of the wherlitic mantle metasomes.