Results 11 to 20 of about 147 (81)

Links between Calcite Kimberlite, Aillikite and Carbonatite in West Greenland: Numeric Modeling of Compositional Relationships [PDF]

open access: yesJournal of Petrology
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

Petrogenesis of a newly discovered ∼1.1 Ga aillikite, carbonate-rich kimberlite, and carbonatite association on the northern margin of the Mid-continental Rift System, Ontario, Canada

open access: yesPrecambrian Research
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]

open access: yesMineralogy and Petrology, 2018
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

open access: yesDoklady Earth Sciences, 2023
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]

open access: yesMinerals, 2020
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

Hydrogen Concentrations and He Isotopes in Olivine From Ultramafic Lamprophyres Provide New Constraints on a Wet Tarim Plume and Earth's Deep Water Cycle

open access: yes, 2022
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

Petrogenesis of Ultramafic Lamprophyres from the Terina Complex (Chadobets Upland, Russia): Mineralogy and Melt Inclusion Composition

open access: yes, 2020
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]

open access: yes, 2008
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.

open access: yes, 1986
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

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