Recent advances are reviewed in the understanding of the geometry and development of
steep, planar normal faults with up to hundreds of meters throw in multilayered sedimentary …

Rapid extension in central Greece is accommodated by large active normal faults that
largely control the geomorphology. The faults bound graben whose asymmetry is evident in …

Preparation of natural hazards maps are vital and essential for urban development. The
main scope of this study is to synthesize natural hazard maps in a single multi-hazard map …

Over 80 new fault plane solutions, combined with satellite imagery as well as both modern
and historical observations of earthquake faulting, are used to investigate the active …

In this paper we examine the connection between the westward motion of Turkey relative to
Europe and the extension in and around the Aegean Sea. The principal new data available …

Extensional tectonism produces characteristic half-graben/tilt-block systems whose facies
mosaics are influenced by tectonically induced slopes resulting from hanging wall …

We present geological and morphological observations at different scales to constrain rates
of faulting and the distribution of deformation in the seismically active Aegean region. We …

Seismicity and fault-plane solutions show that the active deformation in the Adriatic region is
very varied. West of Messina, N—S shortening occurs with slip vectors representative of the …

Relay ramps occur between normal fault segments that overstep in map view. The geometry
and evolution of exposure-scale relay ramps are described from the Somerset coast …

Observations of present-day normal faulting in regions of active continental extension may
be helpful when interpreting the geological record in older extensional basins. The most …