Subduction is the main process that recycles surface material into the mantle. Fluids and
melts derived by dehydration and partial melting reactions of subducted continental crust, a …

Biotite (sensu lato) is a widespread rock‐forming mineral in magmatic rocks that can be
stable in a broad range of pressure and temperature, but appropriate biotite thermometers or …

Abstract Biotite–melt Nb and Ta partition coefficients (DNb and DTa) are crucial for
understanding Nb− Ta enrichment and fractionation in rare metal granites (RMGs) …

Post-collisional mafic magmas are melts of mixed sources formed by the interaction between
crust and mantle. We report the first identification of metasomatic sources formed at> 200 km …

Syncollisional magmatism plays an important but underappreciated role in continental crust
growth and maturation. However, the origin of syncollisional intermediate magmas in …

Dynamic metasomatism experiments were performed by reacting a lamproite melt with
garnet peridotite by drawing melt through the peridotite into a vitreous carbon melt trap …

Abstract The 595–560 Ma post-collisional magmatism in the Alto Pajeú Domain, Borborema
Province, northeastern Brazil, is characterized by the intrusion of voluminous high-K calc …

The mantle is known to be heterogeneous, mainly composed of peridotite and eclogite.
Eclogitederived hydrous melts may interact with harzburgite at the slab-mantle interface in …

Global inventory of shale-oil resources and reserves are far from being complete even in
mature basins which have been intensively drilled and produced and in which the main …

We present major and trace element data on clinopyroxene‐hosted, glassy melt inclusions
(MIs) from a highly enriched (high 87Sr/86Sr= 0.71856) lava (ALIA‐D115‐18) from the …