Results 11 to 20 of about 147 (81)
Links between Calcite Kimberlite, Aillikite and Carbonatite in West Greenland: Numeric Modeling of Compositional Relationships [PDF]
AbstractTextural, mineralogical and mineral compositional observations in a suite of Neoproterozoic aillikite and calcite kimberlite dykes from southern West Greenland point to consistent variations in melt major element compositions amongst these silica-undersaturated magma types.
L H Pilbeam +3 more
openaire +3 more sources
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 ...
Irmak Yılmaz +4 more
openaire +2 more sources
The mantle of Scotland viewed through the Glen Gollaidh aillikite [PDF]
The Glen Gollaidh aillikite dyke (58.36741°N 4.69751°W), N.W. Scotland, occurs within the Neoproterozoic sedimentary rocks of the Moine Supergroup ~4 km east of the Moine Thrust. Phlogopite 40Ar/36Ar measurements give a late Devonian maximum emplacement age of 360.3 ± 4.9 (2σ) Ma. This age occurs in a quiet period of Scottish magmatic history c.
Hutchison, Mark T. +4 more
openaire +3 more sources
Erratum to: U–Pb (ID-TIMS) Age of Garnet from Aillikites of the Kola Alkali Province
An Erratum to this paper has been published: https://doi.org/10.1134 ...
M. V. Stifeeva +5 more
openaire +1 more source
The Newly Discovered Neoproterozoic Aillikite Occurrence in Vinoren (Southern Norway): Age, Geodynamic Position and Mineralogical Evidence of Diamond-Bearing Mantle Source [PDF]
During the period 750–600 Ma ago, prior to the final break-up of the supercontinent Rodinia, the crust of both the North American Craton and Baltica was intruded by significant amounts of rift-related magmas originating from the mantle. In the Proterozoic crust of Southern Norway, the 580 Ma old Fen carbonatite-ultramafic complex is a representative of
Dmitry R. Zozulya +5 more
openaire +1 more source
International audienceWater enters Earth's mantle via subduction of hydrated oceanic slab and largely returns to the ocean-atmosphere system through arc volcanism.
Andrea Giuliani +17 more
core +1 more source
The mineral composition and melt inclusions of ultramafic lamprophyres of the Terina complex were investigated. The rocks identified were aillikites, mela-aillikites, and damtjernites, and they were originally composed of olivine macrocrysts and ...
Ilya Prokopyev +4 more
core +1 more source
Between carbonatite and lamproite—Diamondiferous Torngat ultramafic lamprophyres formed by carbonate-fluxed melting of cratonic MARID-type metasomes [PDF]
New U–Pb perovskite ages reveal that diamondiferous ultramafic lamprophyre magmas erupted through the Archean crust of northern Labrador and Quebec (eastern Canada) between ca.
Tappe, Sebastian +6 more
core +1 more source
Alkaline mafic and ultramafic lamprophyres from the Aillik Bay area, Labrador.
The Aillik Bay lamprophyre dyke swarm comprises abundant sannaites, plus rarer olivine sannaites, aillikites and carbonatites. Sannaites are characterized by phenocrysts of Ti-Al titansalite plus rare olivine and phlogopite in a groundmass dominated by ...
J. Malpas +5 more
core +1 more source

