The Betic-Rif arc is one of the smallest and tightest orogenic arcs on Earth, and together with
its extensional hinterland, the Alborán Domain, it formed between two colliding continents …

Based on previous and new results on partial melting experiments of pyroxenites at high
pressure, we attempt to identify the major element signature of pyroxenite partial melts and …

Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.
However, crustal signatures in the mantle source of basaltic rocks above subduction zones …

The composition of the subcontinental lithospheric mantle (SCLM) is broadly related to the
tectonothermal age of the overlying crust, suggesting a secular change in SCLM-forming …

Differentiation of the Earth's mantle and formation of continental and oceanic crust occur
principally through partial melting and extraction of basaltic melt. Among the mantle rocks …

This paper presents field, petrographic–structural and geochemical data on spinel and
plagioclase peridotites from the southern domain of the Lanzo ophiolitic peridotite massif …

Spinel and garnet pyroxenite xenoliths in Cenozoic basalts from Hannuoba, North China
show extremely heterogeneous chemical and isotopic compositions (εNd=− 27 to+ 34). Most …

The Ronda orogenic peridotite (southern Spain) contains a variety of pyroxene-rich rocks
ranging from high-pressure garnet granulites and pyroxenites to low-pressure plagioclase …

We performed a thermodynamic and experimental study to investigate the fate of pyroxenite-
derived melts during their migration through the peridotitic mantle. We used a simplified …

We report the results of a geochemical study of the Jijal and Sarangar complexes, which
constitute the lower crust of the Mesozoic Kohistan paleo-island arc (Northern Pakistan). The …