Carbonated magmatic sulfide systems: Still or sparkling? [PDF]
Sci AdvCherdantseva M +3 more
europepmc +1 more source
Generation of carbonated peridotite melts via biogenic sediment recycling in modern subduction zones. [PDF]
Sci AdvErrázuriz-Henao C +9 more
europepmc +1 more source
The Crystal Chemistry and Topology of Modular Structures. III. 2D and 3D Zeolites Containing Tetrahedral Layers with the Apophyllite-Type Topology. [PDF]
MoleculesAksenov SM +7 more
europepmc +1 more source
Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab. [PDF]
Nat Commun, 2018 Xu C +10 more
europepmc +1 more source
Trace element partitioning between pyrochlore, microlite, fersmite and silicate melts. [PDF]
Geochem Trans, 2020 Klemme S, Berndt J.
europepmc +1 more source
The effects of local variations in conditions on carbon storage and release in the continental mantle. [PDF]
Natl Sci RevFoley SF, Chen C, Jacob DE.
europepmc +1 more source
Deducing the source and composition of rare earth mineralising fluids in carbonatites: insights from isotopic (C, O, 87Sr/86Sr) data from Kangankunde, Malawi. [PDF]
Contrib Mineral Petrol, 2017 Broom-Fendley S +3 more
europepmc +1 more source
Pyrochlore in Carbonatites, a Key to Understanding Element Mobility in Carbonatite Complexes?
Critical raw materials are more relevant now than ever before, and among these, Niobium and rare earth elements have particularly sensitive supply chains. Most of the world’s Niobium originates from the Alto Paranaiba igneous province of Brazil, where it is found in the mineral Pyrochlore.
openaire +1 more source