Knowledge of temperature at drillable depth is a prerequisite in site selection for geothermal
exploration and development of enhanced geothermal systems (EGS). Equally important …

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

From the analysis of geological, geodetic and geophysical data we provide clear evidence
of seismogenic faults capable of producing large earthquakes in intraplate Europe. Previous …

In this paper we present a review of controlling geological, tectonic and engineering factors
for induced seismicity associated to gas depletion in the Netherlands and we place …

The Cenozoic tectonic evolution of Central Europe was governed over long periods of time
by far-field stresses resulting from continent collision in the Alps (which is still ongoing) ridge …

Paleoseismic analysis of the 10‐km‐long Bree fault scarp in the lower Rhine graben yields
numerous lines of evidence of earthquake activity in the Holocene and late Pleistocene. This …

The West Netherlands Basin (WNB) and the neighbouring Roer Valley Rift System (RVRS)
form the most prominent tectonic features of the onshore Netherlands. The two basins have …

Northern Europe would typically be classified as a relatively stable continental region where
seismic hazard is low. Indeed, in comparison to active zones in the Mediterranean, seismic …

We describe a new numerical approach to constrain the three‐dimensional (3‐D) pattern of
fault reactivation. Taking advantage of the knowledge of the tectonic stress field, the ratio of …

Abstract On April 29, 2017 at 0: 56 UTC (2: 56 local time), an MW= 2.8 earthquake struck the
metropolitan area between Leipzig and Halle, Germany, near the small town of …