Eclogites are witnesses of geodynamic processes that are commonly related to subduction
of oceanic crust. Information on the part of these processes that refers to the burial of this …

A suite of minor and trace elements (Ga, Ti, Ni, Zn, Co, Mn, V, Sc) in chromite grains from
ophiolitic chromitites subjected to high-pressure metamorphism defines a metamorphic …

Chemical signatures of chromitites are commonly used to track the evolution of the Earth's
mantle. However, chemical modification during deformation may have important implications …

Evidence for ultrahigh‐pressure metamorphism (UHPM) in the Rhodope metamorphic
complex comes from occurrence of diamond in pelitic gneisses, variably overprinted by …

The upper mantle rocks of the metamorphosed ophiolite of Chernichevo, Rhodope
Metamorphic Complex in southern Bulgaria, host small chromite ores with unusual …

Remarkably well-preserved crustal sections from the Eastern Hellenides offer the chance to
evaluate the regional geodynamic evolution of continental crust. Here, we identify and …

The specific chemical composition of monazite in shear zones is controlled by the
syndeformation dissolution–precipitation reactions of the rock-forming minerals. This relation …

Abstract The Vertiskos‐Ograzden metamorphic complex (VOC; W‐Rhodope Metamorphic
Domain, RMD) is a key area for reconstructing the geodynamic history of the Hellenides. We …

Linking the deformation history of mylonitized continental rocks to the progress of
devolatilization reactions that trigger reaction softening is critical for the understanding of …

Abstract The Rhodopes in Bulgaria and Greece represent a nappe stack of high-grade units
with polymetamorphic history. Constraining the time of metamorphism in individual subunits …