Voluminous lava flows at Oldoinyo Lengai in 2006: chronology of events and insights into the shallow magmatic system [PDF]
, 2008 BELTON, F +8 more
core +2 more sources
The importance of tectonic setting in assessing European Rare Earth potential [PDF]
, 2014 Rare earth element (REE) resources are commonly found associated with alkaline igneous complexes or carbonatites, or as secondary deposits derived from igneous rocks.
Deady, Eimear +4 more
core
Reply to: Silica is unlikely to be soluble in upper crustal carbonatite melts. [PDF]
Nat Commun, 2023 Berndt J, Klemme S.
europepmc +1 more source
Silicate-carbonate systems with bearing on the origin and crystallization of carbonatites [PDF]
, 1978 Experimental approaches attempt to determine the routes by which crustal carbonatite magmas can be derived from C02-bearing peridotite at high pressures.
Wyllie, P. J.
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On the Feasibility of Imaging Carbonatite-Hosted Rare Earth Element Deposits Using Remote Sensing [PDF]
Rare earth elements (REEs) generate characteristic absorption features in visible to shortwave infrared (VNIR-SWIR) reflectance spectra. Neodymium (Nd) has among the most prominent absorption features of the REEs and thus represents a key pathfinder ...
Black, Martin +6 more
core +1 more source
Detection and Relative Quantification of Neodymium in Sillai Patti Carbonatite Using Decision Tree Classification of the Hyperspectral Data. [PDF]
Sensors (Basel), 2022 Qasim M, Khan SD.
europepmc +1 more source
Island-arc Ankaramites: Primitive Melts from Fluxed Refractory Lherzolitic Mantle [PDF]
, 2017 The distinctive island-arc ankaramites exemplified by the active Vanuatu arc may be produced by melting of refractory lherzolite under conditions in which melting is fluxed by H2O + CO2.
GREEN, D. H. +2 more
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Change in composition and potential functional genes of microbial communities on carbonatite rinds with different weathering times. [PDF]
Front Microbiol, 2022 Chen J +6 more
europepmc +1 more source
Peridotite, kimberlite, and carbonatite explained in the system CaO-MgO-SiO_2-CO_2 [PDF]
, 1975 The key to the origin of carbonatite and kimberlite lies in the system CaO-MgO-SiO_2-CO_2. Increase in pressure causes a carbonation reaction in the peridotite assemblage as follows: forsterite + clinopyroxene + CO_2 ⇌ orthopyroxene + carbonate (Ca:Mg ...
Huang, Wuu-Liang, Wyllie, Peter J.
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