Potassic lavas in the orogenic volcanism of the mediterranean area
Identifieur interne : 000479 ( Istex/Curation ); précédent : 000478; suivant : 000480Potassic lavas in the orogenic volcanism of the mediterranean area
Auteurs : Jörg Keller [Allemagne]Source :
- Journal of Volcanology and Geothermal Research [ 0377-0273 ] ; 1983.
Descripteurs français
- Wicri :
- topic : Essence.
English descriptors
- KwdEn :
- Aeolian, Aeolian island, Aeolian islands, Afyon, Afyon potassic series, Alban hills, Anatolia, Campanian province, Central anatolia, Central italy, Comagmatic, Contrib, Crustal, Crustal contamination, Different degrees, Earth planet, East african rift, Geochemical, Geochemical characteristics, Geodynamic significance, Geol, Hawkesworth, Innocenti, Isotopic composition, Isotopic evidence, John wiley, Keller, Latitic lava, Lava, Magma, Mantle heterogeneities, Mediterranean area, Mediterranean island arcs, Orogenic volcanism, Petrol, Phlegrean fields, Potassic, Potassic lavas, Potassic rocks, Potassic series, Radiogenic isotopes, Roccamonfina volcano, Roman comagmatic region, Shoshonitic, Source mantle, Southern tyrrhenian, Subduction, Tectonic, Tio2, Typical feature, Volcanic, Volcanic area, Volcanic rocks, Volcanism, Volcano, Vollmer, Western anatolia.
- Teeft :
- Aeolian, Aeolian island, Aeolian islands, Afyon, Afyon potassic series, Alban hills, Anatolia, Campanian province, Central anatolia, Central italy, Comagmatic, Contrib, Crustal, Crustal contamination, Different degrees, Earth planet, East african rift, Geochemical, Geochemical characteristics, Geodynamic significance, Geol, Hawkesworth, Innocenti, Isotopic composition, Isotopic evidence, John wiley, Keller, Latitic lava, Lava, Magma, Mantle heterogeneities, Mediterranean area, Mediterranean island arcs, Orogenic volcanism, Petrol, Phlegrean fields, Potassic, Potassic lavas, Potassic rocks, Potassic series, Radiogenic isotopes, Roccamonfina volcano, Roman comagmatic region, Shoshonitic, Source mantle, Southern tyrrhenian, Subduction, Tectonic, Tio2, Typical feature, Volcanic, Volcanic area, Volcanic rocks, Volcanism, Volcano, Vollmer, Western anatolia.
Abstract
Abstract: Volcanism in the Mediterranean fold belts is dominantly related to plate-convergence processes. The occurrence of highly potassic and often leucite-bearing lavas is a typical feature of many Neogene to Quaternary volcanic provinces in the Mediterranean area.The paper describes possible relationships between the Aeolian island arc and the Roman comagmatic region and presents petrological evidence for an ultrapotassic province within the Cypriot-Taurus arc of Turkey. It is thus a contribution to the controversy about tectonic setting and geodynamic significance of the highly potassic volcanism of the Mediterranean suite.
Url:
DOI: 10.1016/0377-0273(83)90014-8
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Potassic lavas in the orogenic volcanism of the mediterranean area</title><author><name sortKey="Keller, Jorg" sort="Keller, Jorg" uniqKey="Keller J" first="Jörg" last="Keller">Jörg Keller</name><affiliation wicri:level="0"><mods:affiliation>Mineralogisches Institut der Universität, D-7800 Freiburg Federal Republic of Germany</mods:affiliation><country wicri:rule="zip">Allemagne</country></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:FCDDBE16B7DC4D08B11A77F1E73D1FE5410FB291</idno><date when="1983" year="1983">1983</date><idno type="doi">10.1016/0377-0273(83)90014-8</idno><idno type="url">https://api.istex.fr/document/FCDDBE16B7DC4D08B11A77F1E73D1FE5410FB291/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000479</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000479</idno><idno type="wicri:Area/Istex/Curation">000479</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">Potassic lavas in the orogenic volcanism of the mediterranean area</title><author><name sortKey="Keller, Jorg" sort="Keller, Jorg" uniqKey="Keller J" first="Jörg" last="Keller">Jörg Keller</name><affiliation wicri:level="0"><mods:affiliation>Mineralogisches Institut der Universität, D-7800 Freiburg Federal Republic of Germany</mods:affiliation><country wicri:rule="zip">Allemagne</country></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Volcanology and Geothermal Research</title><title level="j" type="abbrev">VOLGEO</title><idno type="ISSN">0377-0273</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1983">1983</date><biblScope unit="volume">18</biblScope><biblScope unit="issue">1–4</biblScope><biblScope unit="page" from="321">321</biblScope><biblScope unit="page" to="335">335</biblScope></imprint><idno type="ISSN">0377-0273</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0377-0273</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aeolian</term><term>Aeolian island</term><term>Aeolian islands</term><term>Afyon</term><term>Afyon potassic series</term><term>Alban hills</term><term>Anatolia</term><term>Campanian province</term><term>Central anatolia</term><term>Central italy</term><term>Comagmatic</term><term>Contrib</term><term>Crustal</term><term>Crustal contamination</term><term>Different degrees</term><term>Earth planet</term><term>East african rift</term><term>Geochemical</term><term>Geochemical characteristics</term><term>Geodynamic significance</term><term>Geol</term><term>Hawkesworth</term><term>Innocenti</term><term>Isotopic composition</term><term>Isotopic evidence</term><term>John wiley</term><term>Keller</term><term>Latitic lava</term><term>Lava</term><term>Magma</term><term>Mantle heterogeneities</term><term>Mediterranean area</term><term>Mediterranean island arcs</term><term>Orogenic volcanism</term><term>Petrol</term><term>Phlegrean fields</term><term>Potassic</term><term>Potassic lavas</term><term>Potassic rocks</term><term>Potassic series</term><term>Radiogenic isotopes</term><term>Roccamonfina volcano</term><term>Roman comagmatic region</term><term>Shoshonitic</term><term>Source mantle</term><term>Southern tyrrhenian</term><term>Subduction</term><term>Tectonic</term><term>Tio2</term><term>Typical feature</term><term>Volcanic</term><term>Volcanic area</term><term>Volcanic rocks</term><term>Volcanism</term><term>Volcano</term><term>Vollmer</term><term>Western anatolia</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Aeolian</term><term>Aeolian island</term><term>Aeolian islands</term><term>Afyon</term><term>Afyon potassic series</term><term>Alban hills</term><term>Anatolia</term><term>Campanian province</term><term>Central anatolia</term><term>Central italy</term><term>Comagmatic</term><term>Contrib</term><term>Crustal</term><term>Crustal contamination</term><term>Different degrees</term><term>Earth planet</term><term>East african rift</term><term>Geochemical</term><term>Geochemical characteristics</term><term>Geodynamic significance</term><term>Geol</term><term>Hawkesworth</term><term>Innocenti</term><term>Isotopic composition</term><term>Isotopic evidence</term><term>John wiley</term><term>Keller</term><term>Latitic lava</term><term>Lava</term><term>Magma</term><term>Mantle heterogeneities</term><term>Mediterranean area</term><term>Mediterranean island arcs</term><term>Orogenic volcanism</term><term>Petrol</term><term>Phlegrean fields</term><term>Potassic</term><term>Potassic lavas</term><term>Potassic rocks</term><term>Potassic series</term><term>Radiogenic isotopes</term><term>Roccamonfina volcano</term><term>Roman comagmatic region</term><term>Shoshonitic</term><term>Source mantle</term><term>Southern tyrrhenian</term><term>Subduction</term><term>Tectonic</term><term>Tio2</term><term>Typical feature</term><term>Volcanic</term><term>Volcanic area</term><term>Volcanic rocks</term><term>Volcanism</term><term>Volcano</term><term>Vollmer</term><term>Western anatolia</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Essence</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Volcanism in the Mediterranean fold belts is dominantly related to plate-convergence processes. The occurrence of highly potassic and often leucite-bearing lavas is a typical feature of many Neogene to Quaternary volcanic provinces in the Mediterranean area.The paper describes possible relationships between the Aeolian island arc and the Roman comagmatic region and presents petrological evidence for an ultrapotassic province within the Cypriot-Taurus arc of Turkey. It is thus a contribution to the controversy about tectonic setting and geodynamic significance of the highly potassic volcanism of the Mediterranean suite.</div></front></TEI></record>Pour manipuler ce document sous Unix (Dilib)
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