Calcium isotope compositions as a means to trace carbonate recycling. [PDF]
Huang S, Jacobsen SB.
europepmc +1 more source
Petrogenesis of juvenile pelletal lapilli in ultramafic lamprophyres. [PDF]
Prokopyev I +5 more
europepmc +1 more source
On the interpretation of satellite-derived gravity and magnetic data for studies of crustal geology and metallogenesis [PDF]
Satellite-derived global gravity and magnetic maps have been shown to be useful in large-scale studies of the Earth's crust, despite the relative infancy of such studies.
Hastings, D. A.
core +1 more source
Melting of carbonated pelites at 8-13GPa: generating K-rich carbonatites for mantle metasomatism [PDF]
The melting behaviour of three carbonated pelites containing 0-1wt% water was studied at 8 and 13GPa, 900-1,850°C to define conditions of melting, melt compositions and melting reactions.
Grassi, Daniele, Schmidt, Max
core
Linking deep CO2 outgassing to cratonic destruction. [PDF]
Wang ZX, Liu SA, Li S, Liu D, Liu J.
europepmc +1 more source
Partitioning of REE between calcite and carbonatitic melt containing P, S, Si at 650-900 °C and 100 MPa. [PDF]
Chebotarev DA +2 more
europepmc +1 more source
Experimental production of K-rich metasomes through sediment recycling at the slab-mantle interface in the fore-arc. [PDF]
Gülmez F +4 more
europepmc +1 more source
Assessment of ancylite ore dressability by flotation method
For more than 50 years, most rare earth elements were extracted from carbonatite deposits, which can contain different rare earth phases, but the main extracted minerals are bastnaesite, monazite and xenotime.
Galina V. Mitrofanova +5 more
doaj
Sr-Nd-Pb isotope data for Fuerteventura (Canary Islands) basal complex and subaerial volcanics: applications to magma genesis and evolution [PDF]
Hoernle, Kaj, Tilton, G.
core +1 more source
Speculations on nature and extent of Archean basement in Labrador as indicated by SR, ND and PB isotopic systematics of proterozoic intrusives [PDF]
The Sm-Nd and Rb-Sr isotopic compositions of mid to late Proterozoic (approximately 1.6 to 1.1 Ga) massif-type anorthosites and mafic intrusives in the eastern Canadian shield are correlated with geographic location.
Ashwal, L. D. +2 more
core +1 more source

