Podiform chromitites in the mantle sections of ophiolites belong to either high-Cr
(metallurgical) or high-Al (refractory) varieties. Their highly variable compositions are …

Podiform chromitites have long supplied us with unrivaled information on various mantle
processes, including the peridotite-magma reaction, deep-seated magmatic evolution, and …

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 …

Platinum-group minerals are the dominant control on the budget of platinum-group elements
in ophiolitic chromitites. They vary widely in distribution, morphology, chemistry and Os …

Abstract The southwestern Tianshan (China) metamorphic belt records high-pressure (HP)
to ultrahigh-pressure (UHP) conditions corresponding to a cold oceanic subduction-zone …

Podiform chromitites occur in the meta-dunite horizon of the Dobromirtsi ultramafic massif, in
the Central Rhodope metamorphic core complex (southern Bulgaria). Although these were …

Chromitites, associated with upper mantle peridotites of ophiolites from southeastern Turkey,
are lenticular bodies or veinlets made up of massive, banded and disseminated chromite …

Economically viable chrome ore bodies are hosted within a unit of pervasively serpentinized
harzburgite in the Guleman mine of the homonymous ophiolite in SE Turkey. Chrome ores …

Antigorite is considered as the most important source of water in subduction zones, playing
a key role during arc magma genesis. Although, these magmas seem more oxidized than …

Abstract Trace element (Zn, Co, Mn, Ni, Ga, V, Ti, and Sc) compositions of chromite in mafic-
ultramafic rocks are widely used for addressing their petrogenesis and discriminating …