We present the goals and the current status of the Malargüe seismic array. Our main goal is imaging and monitoring the subsurface below the Malargüe region, Mendoza, Argentina. More specifically, we focus on the Planchon-Peteroa Volcano and an area just east of the town of Malargüe. We start our project installing a temporary array of 38 seismic stations, which records continuously for one year. The array consists of two subarrays: one array located on the flanks of the volcano; the other spread out on a plateau just east of the Andes. The imaging targets, like the Moho and the Nazca slab, are relatively deep. Yet, the array has a dense station spacing, allowing exploration-type processing. For high-resolution imaging, also a dense source s...
The properties of volcanic tremor wavefields at Mt Etna Volcano, Italy, are investigated using data ...
International audienceWe present a new methodology for detection and space-time location of seismic ...
Noise-based seismology is proving to be a complementary ap-proach to active-source or earthquake-bas...
Seismic interferometry (SI) studies the interference phenomenon between pairs of signals in order to...
The Planchón-Peteroa Volcanic Complex (PPVC) is located in the Central Andes, Argentina-Chile. Even ...
The seismic array is part of the Middle America Subduction Experiment (MASE) partnered with Caltech ...
A small aperture quadripartite seismic array was installed on the south-east flanks of Mt. Vesuvius ...
Although the Planchón-Peteroa Volcanic Complex (PPVC) has undergone many hazardous eruptions, only a...
Seismic interferometry (SI) refers to the principle of generating new seismic responses using crossc...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Seismic interferometry (SI) retrieves virtual seismic signals from measurements at two receivers fro...
International audienceNoise-based seismology is proving to be a complementary approach to active-sou...
In the period 2-6 April 2007 a seismic survey was carried out at Solfatara Volcano, (Campi Flegrei, ...
In the present paper we describe the results of a seismic field survey carried out at Copahue Volcan...
The properties of volcanic tremor wavefields at Mt Etna Volcano, Italy, are investigated using data ...
International audienceWe present a new methodology for detection and space-time location of seismic ...
Noise-based seismology is proving to be a complementary ap-proach to active-source or earthquake-bas...
Seismic interferometry (SI) studies the interference phenomenon between pairs of signals in order to...
The Planchón-Peteroa Volcanic Complex (PPVC) is located in the Central Andes, Argentina-Chile. Even ...
The seismic array is part of the Middle America Subduction Experiment (MASE) partnered with Caltech ...
A small aperture quadripartite seismic array was installed on the south-east flanks of Mt. Vesuvius ...
Although the Planchón-Peteroa Volcanic Complex (PPVC) has undergone many hazardous eruptions, only a...
Seismic interferometry (SI) refers to the principle of generating new seismic responses using crossc...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Seismic interferometry (SI) retrieves virtual seismic signals from measurements at two receivers fro...
International audienceNoise-based seismology is proving to be a complementary approach to active-sou...
In the period 2-6 April 2007 a seismic survey was carried out at Solfatara Volcano, (Campi Flegrei, ...
In the present paper we describe the results of a seismic field survey carried out at Copahue Volcan...
The properties of volcanic tremor wavefields at Mt Etna Volcano, Italy, are investigated using data ...
International audienceWe present a new methodology for detection and space-time location of seismic ...
Noise-based seismology is proving to be a complementary ap-proach to active-source or earthquake-bas...