The Torfaj¨okull volcanic system is one of approximately 30 active volcanoes comprising the neovolcanic zones of Iceland. The central volcano of the system is the largest silicic centre in Iceland with a caldera of approximately 12 km diameter. Its high-temperature geothermal\ud system is one of the most powerful in Iceland. Torfaj¨okull is a source of persistent seismicity, where both high- and low-frequency earthquakes occur. To study this microseismicity in detail, a temporary array of 20 broad-band seismic stations was deployed between 2002 June and November. These temporary stations were embedded in the permanent South Iceland Lowland (SIL) network and data from nine adjacent SIL stationswere included in this study.Aminimum one-dimensi...
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geo...
More than 2100 microearthquakes were recorded and crudely located by using data from portable seismo...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
We present relatively relocated earthquake hypocentres for >1000 microearthquakes (ML < 3) that occu...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
The plate boundary between the American and Eurasian plates runs in southwest Iceland along a 5-10 k...
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geo...
Microearthquake hypocenters were analysed in the Krýsuvík geothermal area in SW-Iceland with data ta...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geo...
More than 2100 microearthquakes were recorded and crudely located by using data from portable seismo...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
The main goal of this Ph.D. thesis is to improve locations of earthquake hypocenters and to resolve ...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
We present relatively relocated earthquake hypocentres for >1000 microearthquakes (ML < 3) that occu...
Geothermal systems in the Hengill volcanic area, SW Iceland, started to be exploited for electrical ...
The plate boundary between the American and Eurasian plates runs in southwest Iceland along a 5-10 k...
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geo...
Microearthquake hypocenters were analysed in the Krýsuvík geothermal area in SW-Iceland with data ta...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geo...
More than 2100 microearthquakes were recorded and crudely located by using data from portable seismo...
Seismicity was monitored beneath the Krafla central volcano, NE Iceland, between 2009 and 2012 durin...