seismic reflection, volcano-/tectono-magmatic activity, seismotectonic behavior, hybrid events, harmonic tremors. ABSTRACT This study presents a methodological and conceptual approach to effectively consider the Lake Van volcanic basin and its seismicity relationships by using seismic reflection and three-component velocity seismogram data. We used a couple of data set with high resolution geochirp and multi-channel seismic reflection data collected all over the Lake Van basin. Lake-wide seismicity analysis are reconsidered by spectral analysing of KOERI earthquake data, seismic waveforms at VANB broadband station. Thus, we improved the efficiency of our data set to understand and explain the volcano-related seismicity and advanced our inpu...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...
Central Anatolia has been characterized by active volcanism since ∼10 Ma which created the so called...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...
The structural evolution of Lake Van Basin, eastern Turkey, was reconstructed based on seismic refle...
This paper presents results of a multi-channel seismic reflection survey at Lake Van and provides co...
Analysis of multi-channel seismic reflection and chirp data from Lake Van (eastern Turkey) reveals v...
This study analyzed multi-channel seismic reflection data from Lake Van, Eastern Anatolia, to provid...
More than 1500 km of multi-channel seismic reflection profiles combined with ICDP (International Con...
EGU2011-1847-3 Lake Van is a lake by volume of 607 km3 and a maximum depth of 450 meters in a tecto...
The 23 October 2011 Van earthquake took place in the NE part of Lake Van area, surprisingly on a fau...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
Kawah Ijen (2386 m) is a stratovolcano located within Ijen Caldera, at the easternmostpart of Java i...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
We provide a complete description of the characteristics of excitation and attenuation of the ground...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...
Central Anatolia has been characterized by active volcanism since ∼10 Ma which created the so called...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...
The structural evolution of Lake Van Basin, eastern Turkey, was reconstructed based on seismic refle...
This paper presents results of a multi-channel seismic reflection survey at Lake Van and provides co...
Analysis of multi-channel seismic reflection and chirp data from Lake Van (eastern Turkey) reveals v...
This study analyzed multi-channel seismic reflection data from Lake Van, Eastern Anatolia, to provid...
More than 1500 km of multi-channel seismic reflection profiles combined with ICDP (International Con...
EGU2011-1847-3 Lake Van is a lake by volume of 607 km3 and a maximum depth of 450 meters in a tecto...
The 23 October 2011 Van earthquake took place in the NE part of Lake Van area, surprisingly on a fau...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
Kawah Ijen (2386 m) is a stratovolcano located within Ijen Caldera, at the easternmostpart of Java i...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
We provide a complete description of the characteristics of excitation and attenuation of the ground...
The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...
Central Anatolia has been characterized by active volcanism since ∼10 Ma which created the so called...
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated se...