Asymmetric caldera-related structures in the area of the Avacha group of volcanoes in Kamchatka as revealed by ambient noise tomography and deep seismic sounding

• Published in: Journal of Volcanology and Geothermal Research
• Main Authors: Koulakov, Ivan, Jaxybulatov, Kayrly, Shapiro, Nikolay M., Abkadyrov, Ilyas, Deev, Evgeny, Jakovlev, Andrey, Kuznetsov, Pavel, Gordeev, Evgeny, Chebrov, Viktor
• Other Authors: Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2014
• Subjects: Kamchatka; Avachinsky volcano; Ambient noise tomography; Deep seismic sounding; Caldera forming; [SDU]Sciences of the Universe [physics]; Avacha; Petropavlovsk; Petropavlovsk-Kamchatsky
• Online Access: https://hal-insu.archives-ouvertes.fr/insu-03581097; https://doi.org/10.1016/j.jvolgeores.2014.08.012

International audience Avacha group includes two active and potentially dangerous volcanoes, Avachinsky and Koryaksky, located close to Petropavlovsk-Kamchatsky, the main city of Kamchatka. We present the results of two independent seismic studies of shallow crustal structures beneath the Avacha group based on passive and active source observations. The first study is based on the analysis of continuous recording by 11 seismic stations installed over the Avacha group in 2012 and 7 permanent stations in the same region. We present a series of 2D Rayleigh-wave group velocity maps based on correlation of ambient noise, that were then converted into 3D distribution of shear wave velocity. The second work was based on the reprocessing of an active source deep seismic sounding profile across the Avachinsky volcano that was shot in 1982-1984. We made the analysis of travel times of refracted waves using a 2D tomography inversion. The resulting seismic models appear to be consistent with each other and show clear low-velocity zone to the SW of the Avachinsky volcano and high velocity structures to NE. These observations also agree with the existing gravity and magnetotelluric measurements. Based on the obtained seismic models we identify two large buried calderas and large lava flows that are thought to be related to a series of large eruption episodes of Avachinsky occurred within the last 30,000 years.