The earthquake map of Denmark is constantly being improved. Together with data from western Sweden and southern Norway it shows more and more convincingly a gradual, scattered earthquake activity across the Kattegat region from low activity in the Precambrian basement of Scandinavia to lack of earthquakes in south-western Denmark and northern Germany. The activity is only partly connected with mapped geological features
We review the results of the TopoScandiaDeep project, a component of the TOPOEUROPE project, in whic...
The best available rebound model is used to investigate the role that postglacial rebound plays in t...
century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of ML(UPP)=4...
Assessment of earthquake hazard is improved if geological and geodetic data are included in addition...
The Geological Survey of Denmark and Greenland (GEUS) records seismological data at six locations in...
The occurrence of earthquakes in southern Scandinavia including Denmark 1900-1950 is considered in r...
Recent Danish seismological projects involving neotectonic investigations and structural studies hav...
A moderately strong earthquake struck southern Sweden 5 km south-west of the town of Sjöbo, 60 km ea...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
The mechanism of support for the present topography of Scandinavia is not well explained by current ...
The Sorgenfrei-Tornquist Zone (STZ) is the northwestern segment of the Tornquist Zone and extends fr...
The double difference earthquake relocation method (DD) is used to improve the seismicity image for ...
The Chalk Group is ubiquitous in the subsurface of the Danish Basin and its upper levels are exposed...
We review the results of the TopoScandiaDeep project, a component of the TOPOEUROPE project, in whic...
The best available rebound model is used to investigate the role that postglacial rebound plays in t...
century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of ML(UPP)=4...
Assessment of earthquake hazard is improved if geological and geodetic data are included in addition...
The Geological Survey of Denmark and Greenland (GEUS) records seismological data at six locations in...
The occurrence of earthquakes in southern Scandinavia including Denmark 1900-1950 is considered in r...
Recent Danish seismological projects involving neotectonic investigations and structural studies hav...
A moderately strong earthquake struck southern Sweden 5 km south-west of the town of Sjöbo, 60 km ea...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
The mechanism of support for the present topography of Scandinavia is not well explained by current ...
The Sorgenfrei-Tornquist Zone (STZ) is the northwestern segment of the Tornquist Zone and extends fr...
The double difference earthquake relocation method (DD) is used to improve the seismicity image for ...
The Chalk Group is ubiquitous in the subsurface of the Danish Basin and its upper levels are exposed...
We review the results of the TopoScandiaDeep project, a component of the TOPOEUROPE project, in whic...
The best available rebound model is used to investigate the role that postglacial rebound plays in t...
century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of ML(UPP)=4...