Shapiro, N. M.; Sens-Schönfelder, C.; Lühr, B.G.; Weber, M.; Abkadyrov, I.; Gordeev, E. I.; Koulakov, I.; Jakovlev, A.; Kugaenko, Y. A.; Saltykov, V. A. (2015): Klyuchevskoy volcanic group experiment (KISS). GFZ Data Services. Other/Seismic Network. doi:10.14470/K47560642124.
Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Sciences, Petropavlovsk-Kamchatsky, Russia; Kamchatka Branch of the Geophysical Survey, Russian Academy of Sciences, Petropavlovsk-Kamchatsky, Russia; Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences and Novosibirsk State University, Novosibirsk, Russia; Institut de Physique du Globe de Paris, Paris, France; GFZ German Research Centre for Geosciences, Potsdam, Germany
Shapiro, N. M.; Sens-Schönfelder, C.; Lühr, B.G.; Weber, M.; Abkadyrov, I.; Gordeev, E. I.; Koulakov, I.; Jakovlev, A.; Kugaenko, Y. A.; Saltykov, V. A.
Klyuchevskoy volcanic group experiment (KISS)
The KISS network was installed in the frame of the "Klyuchevskoy Investigation - Seismic Structure of an extraordinary volcanic system" project and recorded data between summer 2015 and summer 2016 in one of the world's largest clusters of subduction volcanoes - the Klyuchevskoy volcanic group (KVG). It is located in eastern Russia at the northern end of the Kuril-Kamchatka subduction zone close to its intersection with the Aleutian arc and the north-western termination of Hawaii-Emperor seamount chain. Additional to the 4700m high Mount Klyuchevskoy the KVG contains 12 other volcanoes that have together erupted about 1 cubic meter rock per second averaged over the past 10,000 years. Among those Klyuchevskoy, Bezymianny and Tolbachik were the most active ones during the last decades with eruptions styles ranging from explosive to Hawaiian-type. The KISS experiment is designed to investigate the volcanic and seismic processes and its structural setting in the KVG. The network covers a circular region of about 80km diameter with some linear extensions. It includes data from 77 temporary seismic stations with broadband and short period sensors that were installed on concrete plates in about 60cm deep holes. Due to the local conditions the stations were battery powered and could not be serviced during the experiment. GPS reception of the digitizers was not continuous at all stations due to thick snow cover and vegetation. Waveform data are available from the GEOFON data centre, under network code X9, and are embargoed until end of 2019.
* Description is taken from seismic metadata, and may not match the preferred title for citations.
Green, R. G.; Sens‐Schönfelder, C.; Shapiro, N.; Koulakov, I.; Tilmann, F.; Dreiling, J.; … Gordeev, E. (2020). Magmatic and Sedimentary Structure beneath the Klyuchevskoy Volcanic Group, Kamchatka, From Ambient Noise Tomography. Journal of Geophysical Research: Solid Earth, 125(3). doi:10.1029/2019jb018900
Shapiro, N. M.; Sens-Schönfelder, C.; Lühr, B.G.; Weber, M.; Abkadyrov, I.; Gordeev, E. I.; Koulakov, I.; Jakovlev, A.; Kugaenko, Y. A.; Saltykov, V. A. (2017). Understanding Kamchatka’s extraordinary volcano cluster. Eos, 98. doi:10.1029/2017EO071351