Deformations formed in unconsolidated sediments are known as soft-sediment deformation
structures. Their nature, the time of their genesis, and the state in which the sediments …

Late Pleistocene glaciolacustrine sediments in the northern part of Estonia show a wide
spectrum of ductile and brittle deformation structures like:(1) injection structures, dish …

The main types of seismites are reviewed following the proposed classification and are
illustrated by our own case studies. The large variety of seismites, depends on the …

Paleoseismic studies of two historically aseismic Quaternary faults in Australia confirm that
cratonic faults in stable continental regions (SCR) typically have a long-term behavior …

Five main deformation units, discrete sheets of deformed sediments that lie between a
significant thickness of undeformed sediment, were selected for study within Late …

The Plio-Pleistocene Zarzal Formation corresponds to fluvio-lacustrine sediments deposited
in an intramontane depression within the Colombian Andes, associated with the Cauca …

As part of a paleoseismological investigation along the Bree fault scarp (western border of
the Roer Graben), various geophysical methods [electrical profiling, electromagnetic (EM) …

Abstract The East Anatolian Fault System (EAFS) is a 30-km-wide, 700-km-long and NE-
trending sinistral strike-slip megashear belt between the Anatolian platelet in the northwest …

Recognising of tectonic deformations in Quaternary sediments is important for interpretating
palaeoclimatic developments accurately. Distinguishing deformations caused by seismic …

We provide a synthesis of the long-term earthquake activity in the region of northwest
Europe between the Lower Rhine Embayment and the southern North Sea. Reevaluated …