Results 81 to 90 of about 127 (117)
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Geochemistry and petrology of ultramafic lamprophyres from Schirmacher Oasis, East Antarctica
Mineralogy and Petrology, 1999Petrographic and geochemical data are presented for some ouachitites from the Schirmacher Oasis. The studied dike intruded into the metamorphic basement of the East Antarctic craton. The ouachitite samples contain substantial amounts of zoned phlogopite and diopsidic to salitic pyroxene as phenocrysts.
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Geologische Rundschau, 1981
Alkahne ultramafic lamprophyres and associated carbonatite dykes form north-south trending dyke swarms. The lamprophyres are sub-divided into micaceous, picritic and breccia varieties. Carbonatites sensu stricto (beforsites) occur very subordinate.
Peter Kresten +2 more
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Alkahne ultramafic lamprophyres and associated carbonatite dykes form north-south trending dyke swarms. The lamprophyres are sub-divided into micaceous, picritic and breccia varieties. Carbonatites sensu stricto (beforsites) occur very subordinate.
Peter Kresten +2 more
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Lithos, 2017
Abstract Carbonate-rich ultramafic lamprophyres (aillikites) and associated rocks characteristically occur during the early stages of thinning and rifting of cratonic mantle lithosphere, prior to the eruption of melilitites, nephelinites and alkali basalts.
Marina Veter +3 more
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Abstract Carbonate-rich ultramafic lamprophyres (aillikites) and associated rocks characteristically occur during the early stages of thinning and rifting of cratonic mantle lithosphere, prior to the eruption of melilitites, nephelinites and alkali basalts.
Marina Veter +3 more
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Contributions to Mineralogy and Petrology, 2018
We studied olivines from the Devonian pre-trap (the Ilbokich occurrence) and the Triassic post-trap (the Chadobets occurrence) carbonate-rich ultramafic lamprophyres (UMLs) in the southwestern portion of the Siberian craton. On the basis of detailed investigations of major, minor, and trace-element distributions, we have reconstructed the main ...
A. A. Nosova +5 more
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We studied olivines from the Devonian pre-trap (the Ilbokich occurrence) and the Triassic post-trap (the Chadobets occurrence) carbonate-rich ultramafic lamprophyres (UMLs) in the southwestern portion of the Siberian craton. On the basis of detailed investigations of major, minor, and trace-element distributions, we have reconstructed the main ...
A. A. Nosova +5 more
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Petrogenesis of ultramafic lamprophyres and carbonatites of the Alnö complex (central Sweden)
Goldschmidt2022 abstracts, 2022Lukáš Krmíček +4 more
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Russian Geology and Geophysics
Abstract ––The paper presents data on the age and composition of phlogopite from dikes of ultramafic lamprophyres (aillikites) of the Zima Complex located within the Urik–Iya graben in the East Sayan region (southern margin of the Siberian craton).
Ya.N. Nugumanova +3 more
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Abstract ––The paper presents data on the age and composition of phlogopite from dikes of ultramafic lamprophyres (aillikites) of the Zima Complex located within the Urik–Iya graben in the East Sayan region (southern margin of the Siberian craton).
Ya.N. Nugumanova +3 more
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ALTERATION IN ULTRAMAFIC LAMPROPHYRES AND ITS CONTROL ON REE DISTRIBUTION IN WESTERN KENTUCKY
Geological Society of America Abstracts with Programs, 2023Zachary Walton +2 more
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International Geology Review, 2016
ABSTRACTLate Jurassic ultramafic lamprophyre (UML) sills and dikes occur as 3 km-long intrusions within the allochthonous Whara Formation of the Batain nappes, eastern Oman. The sills and dikes comprise macrocrystic phlogopite and spinel-bearing aillikite and damtjernite.
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ABSTRACTLate Jurassic ultramafic lamprophyre (UML) sills and dikes occur as 3 km-long intrusions within the allochthonous Whara Formation of the Batain nappes, eastern Oman. The sills and dikes comprise macrocrystic phlogopite and spinel-bearing aillikite and damtjernite.
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Alkaline and ultramafic lamprophyres in Italy: Distribution, mineral phases, and bulk rock data
2008Several lamprophyre outcrops occur in Italy paralleling the European cycles. Lamprophyre occurrences from the lower Cretaceous to the Oligocene are comprised primarily of dykes and rarely lavas, generally emplaced in isolation. They are ultramafic or alkaline lamprophyres located in eight different places ranging from the eastern Alps to the areas of ...
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