Neotethyan suprasubduction zone ophiolites represent anomalous oceanic crust developed
in older host basins during trench rollback cycles and later entrapped in orogenic belts as a …

A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of orogens,
including the substrate of the Pannonian and Transylvanian basins, is presented in the form …

Ongoing seafloor exploration highlights that ultramafic-hosted seafloor massive sulfide
deposits (UM-SMS) are ubiquitous along slow to ultra-slow spreading ridges. These …

The Eastern Mediterranean region exhibits a fascinating diversity of ophiolites and related
oceanic magmatic units of mainly Triassic, Jurassic and Cretaceous age. Comparisons with …

In this paper, a new discrimination diagram using absolute measures of Th and Nb is
applied to post-Archean ophiolites to best discriminate a large number of different ophiolitic …

Suprasubduction zone (SSZ) ophiolites in orogenic belts represent oceanic crust generation
in subduction rollback cycles during the closing stages of basins prior to terminal continental …

The Middle Jurassic Mirdita Ophiolite in northern Albania is part of an ophiolite belt
occurring between the Apulian and Pelagonian subcontinents in the Balkan Peninsula. The …

Diamonds and a wide range of unusual minerals were originally discovered from the
chromitite and peridotite of the Luobusa ophiolite along the Yarlong–Zangbu suture zone in …

All the geological constraints for an exhaustive reconstruction of the Triassic to Tertiary
tectonic history of the southern Dinaric-Hellenic belt can be found in Albania and Greece …

The tectonic history and time of closure of the Palaeo-Asian ocean of the Altaids are issues
of lively current debate. To address these issues, this paper presents detailed geological …