Results 61 to 70 of about 296 (107)
In this study, we present new field, petrographic, and whole-rock major and trace element, and Nd–Pb–Sr radiogenic isotope data for a newly discovered aillikite, carbonate-rich kimberlite, and carbonatite association on the northern shore of Lake ...
Robert Frei, Ali Polat
exaly +4 more sources
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Doklady Earth Sciences
This study presents petrographic and mineral chemical data for olivine in aillikites from the Namuaiy pipe intruded into the Khibiny Massif, the Kola Alkaline Carbonatite Province.
Andrei Arzamastsev +2 more
exaly +3 more sources
This study presents petrographic and mineral chemical data for olivine in aillikites from the Namuaiy pipe intruded into the Khibiny Massif, the Kola Alkaline Carbonatite Province.
Andrei Arzamastsev +2 more
exaly +3 more sources
Lithos, 2009
A regional study of dike and sill occurrences of kimberlitic rocks in terms of xenolith and megacryst assemblages from the diamond province in southern West Greenland demonstrates very systematic variation in the composition of melts across the margin of the Archaean core of the North Atlantic craton.
Karina K. Sand +2 more
exaly +3 more sources
A regional study of dike and sill occurrences of kimberlitic rocks in terms of xenolith and megacryst assemblages from the diamond province in southern West Greenland demonstrates very systematic variation in the composition of melts across the margin of the Archaean core of the North Atlantic craton.
Karina K. Sand +2 more
exaly +3 more sources
Canadian Journal of Earth Sciences, 2000
A dozen ultramafic lamprophyre dykes have been identified in the eastern part of Ungava Bay, Québec. The dark grey dykes are composed of macrocrysts of olivine and phlogopite featuring tetraferriphlogopite rims. These minerals are included in a matrix consisting of fine-grained phlogopite, olivine, spinel, and interstitial carbonate.
S. Digonnet +4 more
exaly +3 more sources
A dozen ultramafic lamprophyre dykes have been identified in the eastern part of Ungava Bay, Québec. The dark grey dykes are composed of macrocrysts of olivine and phlogopite featuring tetraferriphlogopite rims. These minerals are included in a matrix consisting of fine-grained phlogopite, olivine, spinel, and interstitial carbonate.
S. Digonnet +4 more
exaly +3 more sources
Lithos, 2009
Abstract We discuss mineral chemistry data and report ten high-precision U–Pb (zircon, baddeleyite, pyrochlore, and perovskite) and Rb–Sr phlogopite ages for the newly discovered Tikiusaaq carbonatite intrusion and associated ultramafic dykes from the North Atlantic craton, West Greenland.
Antonio Simonetti +2 more
exaly +3 more sources
Abstract We discuss mineral chemistry data and report ten high-precision U–Pb (zircon, baddeleyite, pyrochlore, and perovskite) and Rb–Sr phlogopite ages for the newly discovered Tikiusaaq carbonatite intrusion and associated ultramafic dykes from the North Atlantic craton, West Greenland.
Antonio Simonetti +2 more
exaly +3 more sources
First Discovery of Paleoproterozoic Aillikite Dikes in Sarmatia: Geochemistry and Petrogenesis
Doklady Earth SciencesRoman Terentiev +2 more
exaly +3 more sources
To provide new insights into the origin and evolution of ultramafic lamprophyres (UMLs) and their mantle source, we examined two UML (aillikite and damtjernite) occurrences of different ages in the western portion of the Siberian Craton (Ilbokich and ...
Adam Abersteiner, A A Nosova, D S Yudin
exaly +3 more sources
Inwards-Younging of the Annular Twihinate Carbonatite-Aillikite Complex (Southern Morocco)
Goldschmidt2025 abstractsLucas Tatnell +7 more
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The Late Cretaceous Mata da Corda Formation, located in the eastern part of the Alto Paranaíba Igneous Province (APIP), Central Brazil, is one of the few places on Earth where kamafugite melts reached the surface generating large volumes of lava ...
Felipe Velásquez Ruiz +6 more
semanticscholar +3 more sources
Kimberlites and aillikites as probes of the continental lithospheric mantle
Lithos, 2009ARTICLE I NFO Although the mantle xenoliths carried by kimberlites are the source of much of our information about the composition of the mantle beneath the continents, the compositions of kimberlites themselves have received little attention for the information they carry about the nature of the lithospheric mantle. This neglect in part reflects their
D. Francis, M. Patterson
semanticscholar +2 more sources

