Chemical geodynamics is an integrated discipline that studies the geochemical structure
and tectonic evolution of geospheres with the aim of linking tectonic processes to …

At subduction zones, crustal material enters the mantle. Some of this material, however, is
returned to the overriding plate through volcanic and plutonic activity. Magmas erupted …

We experimentally investigated phlogopite-and C–O–H-bearing lherzolite to model the
mantle wedge fluxed by volatiles released from a subducting crustal slab. Experiments have …

Subduction zones have been the focus of many studies since the advent of plate tectonics in
1960s. Workings within subduction zones beneath volcanic arcs have been of particular …

We present two case studies of metasomatised garnet peridotite from the Sulu (Zhimafang)
and of garnet orthopyroxenite from the Dabie Shan (Maowu) ultrahigh-pressure terranes …

Processes taking place in subduction zones are the main controller of the chemical cycle of
volatile and incompatible elements in the Earth system. Metamorphic devolatilization …

Lithospheric slices preserving pre-Alpine metamorphic imprints are widely described in the
Alps. The Variscan parageneses recorded in continental, oceanic, and mantle rocks suggest …

This study concentrates on small intrusions along two important faults of the Giudicarie fault
system, the Northern Giudicarie and the Meran-Mauls fault, summarised under the term …

A new lithotype of peridotite, phlogopite-and apatite-bearing spinel–garnet peridotite,
associated with leucocratic granulite, has been recognized at the Plešovice quarry in the …

We document the presence of dolomite±apatite in orogenic peridotites from the Ulten Zone
(UZ, Italian Alps), the remnants of a Variscan mantle wedge tectonically coupled with …