Abstract The Gulf of Lion margin is one of the Tertiary extensional basins of the western
Mediterranean that opened during convergence of Africa and Europe. This Oligocene …

Age and rock type, regional distribution and structural setting of volcanic and plutonic
manifestations from the western Mediterranean basin and peripheral orogens during the …

Italian Plio-Quaternary magmatism exhibits a very wide petrological, geochemical and
radiogenic-isotope variability, which makes magma genesis and geodynamic significance …

Metamorphic core complexes of the Aegean region have revealed midcrustal, shallow‐
dipping extensional shear zones. These shear zones display constant kinematic indicators …

The Apennines fold-thrust belt has developed over the past∼ 20 my in response to
southeastward retrograde migration of the Adriatic trench in a region of ongoing subduction …

В монографии с позиций тектонофизики обобщены результаты изучения строения,
механизмов формирования и эволюции разрывных сетей в разноранговых разломных …

Abstract The Betic-Rif arcuate mountain belt (southern Spain, northern Morocco) has been
interpreted as a symmetrical collisional orogen, partly collapsed through convective removal …

A seismically active low-angle normal fault is recognized at depth in the Northern
Apennines, Italy, where recent exhumation has also exposed ancient examples at the …

We present seismological evidence for the existence of an actively slipping low‐angle
normal fault (15° dip) located in the northern Apennines of Italy. During a temporary seismic …

Six moderate magnitude earthquakes (5< Mw< 6) ruptured normal fault segments of the
southern sector of the North Apennine belt (central Italy) in the 1997 Colfiorito earthquake …