Large parts of the Mediterranean were formed during the Mesotethys Ocean opening and
subsequently became land-locked in the midst of the Africa-Eurasia plate convergence …

Subduction of oceanic crust into the mantle results in the relatively young Mesozoic–
Cenozoic age of the current oceanic basins, thus, hindering our knowledge of ancient …

Deep and long-lived rifted basins host valuable information about tectonic evolution and
environmental changes occurring in their surroundings throughout hundreds of millions of …

Recent giant gas discoveries within deeply buried structural highs in the middle of the
Levant basin have attracted the attention of the industrial and academic communities striving …

The Earth's crust is exceptionally important to understand the geological evolution of our
planet and to access natural resources as minerals, critical raw materials, geothermal …

The recent 2016–2017 seismic sequence in Central Italy has prompted the investigation of
several geological and geophysical data in order to derive more accurate subsurface …

ABSTRACT The Central‐Eastern Mediterranean region is known to be a complex area due
to the interaction of four tectonic plates, namely Arabia, Africa, Anatolia and Eurasia, and by …

The Yinkeng orefield is located in the eastern Nanling region, South China. The Nanling
region hosts numerous W (-Sn)-dominant, polymetallic deposits related to the widely …

The interpretation of five 2D PSTM seismic reflection sections (14 s TWT) covering the
northern Levant Basin revealed a total of 10 horizons, among which, one is interpreted as an …

Interpretations of the tectonic setting of the Nile Delta of Egypt and its offshore extension are
challenged by the thick sedimentary cover that conceals the underlying structures and by the …