A moderately strong earthquake struck southern Sweden 5 km south-west of the town of Sjöbo, 60 km east of Malmö, in the early morning at 6:20 a.m. local time on 16 December 2008. The epicentre was located in Skåne, a region that is known for its extremely low seismicity, and its location was determined to be 55.5°N and 13.6°E with an uncertainty of about 6 km. A depth of 9 km with an uncertainty of 3 km was obtained from teleseismic observations at the Yellowknife seismic array, USA. Since waveform data from the Swedish national seismic network are not yet available, depth estimation using local stations has so far not been attempted. During the period 1970–2008, only three small earthquakes were detected in the region; the largest measured...
A new seismic reflection survey for imaging deeper levels of the end-glacial Parvie fault system in ...
Earthquakes have only on a few occasions exceeded magnitude 4 in Sweden in modern times. The safety ...
This investigation examines the contemporary documentation of a sequence of low-magnitude earthquake...
The Geological Survey of Denmark and Greenland (GEUS) records seismological data at six locations in...
century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of ML(UPP)=4...
The occurrence of earthquakes in southern Scandinavia including Denmark 1900-1950 is considered in r...
© The Author 2015. Published by Oxford University Press on behalf of The Royal Astronomical Society....
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
© 2015 Author(s). A new seismic reflection survey for imaging deeper levels of the end-glacial Pärvi...
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...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
Assessment of earthquake hazard is improved if geological and geodetic data are included in addition...
A new seismic reflection survey for imaging deeper levels of the end-glacial Parvie fault system in ...
Earthquakes have only on a few occasions exceeded magnitude 4 in Sweden in modern times. The safety ...
This investigation examines the contemporary documentation of a sequence of low-magnitude earthquake...
The Geological Survey of Denmark and Greenland (GEUS) records seismological data at six locations in...
century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of ML(UPP)=4...
The occurrence of earthquakes in southern Scandinavia including Denmark 1900-1950 is considered in r...
© The Author 2015. Published by Oxford University Press on behalf of The Royal Astronomical Society....
During the late or post Weichselian glacial periods, about 9500 years ago, several faulting associat...
© 2015 Author(s). A new seismic reflection survey for imaging deeper levels of the end-glacial Pärvi...
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...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
By studying the frequency domain of seismic signals generated by earthquakes, the source parameters ...
Assessment of earthquake hazard is improved if geological and geodetic data are included in addition...
A new seismic reflection survey for imaging deeper levels of the end-glacial Parvie fault system in ...
Earthquakes have only on a few occasions exceeded magnitude 4 in Sweden in modern times. The safety ...
This investigation examines the contemporary documentation of a sequence of low-magnitude earthquake...