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
Sm-Nd Isotopic Studies of Ureilite Novo Urei [PDF]
Ureilites are ultramafic (harzburgitic) achondrites composed predominantly of olivine and pyroxenes, abundant carbon (graphites and shock-produced diamonds), some metal and sulfides.
Goodrich, C. A. +3 more
core +1 more source
The article presents the results of a comprehensive study of diamondiferous lherzolite from the V.Grib kimberlite pipe. The composition of rock-forming minerals (olivine, orthopyroxene, Cr-diopside, Cr-pyrope) in terms of major elements mainly ...
Elena V. Agasheva +2 more
doaj
Effects of water content, temperature and pressure on actinide tracer diffusion in melts of haplogranitic composition [PDF]
Dingwell, Donald B., Mungall, Jim
core +1 more source
CRATONIC PERIDOTITES AND SILICA-RICH MELTS: DIOPSIDE-ENSTATITE RELATIONSHIPS IN POLYMICT XENOLITHS, KAAPVAAL, SOUTH AFRICA [PDF]
Gurney, J J +3 more
core +1 more source
Cluster analysis reveals increasing plume-like magmatism during progressive rifting in Afar (Ethiopia). [PDF]
Tortelli G +5 more
europepmc +1 more source
Mantle-derived fluid flux controls Olympic Dam-style Fe oxide-Cu-Au mineralisation. [PDF]
Thiel S +4 more
europepmc +1 more source
Discovery of a heavy silicon isotope mantle reservoir. [PDF]
Liu MR +16 more
europepmc +1 more source
Channelized metasomatism in Archean cratonic roots as a mechanism of lithospheric refertilization. [PDF]
Roots EA +6 more
europepmc +1 more source

