Paleogeography is the study of the changing surface of Earth through time. Driven by plate
tectonics, the configuration of the continents and ocean basins has been in constant flux …

Across the entire mantle we interpret 94 positive seismic wave-speed anomalies as
subducted lithosphere and associate these slabs with their geological record. We document …

Carboniferous sandstone within the Paleo-Mesomediterranean Domain (Malaguide
Subdomain), in southern Spain, represents a key detrital mode within the sedimentary …

We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …

The making of Pangea is the result of large-scale amalgamation of continents and micro-
continents, which started at the end of the Neoproterozoic with the formation of Gondwana …

This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

A new reconstruction of Alpine Tethys combines plate-kinematic modelling with a wealth of
geological data and seismic tomography to shed light on its evolution, from sea-floor …

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 …

The Anarak, Jandaq and Posht-e-Badam metamorphic complexes occupy the NW part of the
Central-East Iranian Microcontinent and are juxtaposed with the Great Kavir block and …

Along the northern border of Africa, Pangea breakup has been diachronic. During the
Jurassic, the Alpine Tethys propagated northeastward from the Atlantic to the Alps. During …