FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2067396832> ?p ?o ?g. }

• W2067396832 endingPage "33" @default.
• W2067396832 startingPage "17" @default.
• W2067396832 abstract "The volcanic arc of the Hellenic subduction zone with its four volcanic centers is of major relevance when evaluating the seismovolcanic hazard for the Aegean region. We present results from a 22-station temporary seismic network (CYCNET) in the central Hellenic Volcanic Arc (HVA). CYCNET recordings allow to analyze the level and spatio-temporal evolution of microseismic activity in this region for the first time. A total of 2175 events recorded between September 2002 and July 2004 are analyzed using statistical methods, cluster analysis and relative relocation techniques. We identify distinct regions with significantly varying spatio-temporal behavior of microseismicity. A large portion of the seismic activity within the upper crust is associated with the presence of islands representing horst structures that were generated during the major Oligocene extensional phase. In contrast, the central part of the Cyclades metamorphic core complex remains aseismic considering our magnitude threshold of 1.8 except one spot where events occur swarm-like and with highly similar waveforms. The highest activity in the study area was identified along the SW–NE striking Santorini–Amorgos zone. Within this zone the submarine Columbo volcano exhibits strong temporal variations of seismic activity on a high background level. This activity is interpreted to be directly linked to the magma reservoir and therein the migration of magma and fluids towards the surface. NE of Columbo where no volcanic activity has yet been reported we observe a similar seismicity pattern with small-scaled activity spots that might represent local pathways of upward migrating fluids or even developing volcanic activity within this zone of crustal weakness. In contrast, the Santorini and Milos volcanic complexes do not show significant temporal variations and low to moderate background activity, respectively. Relating our results to the distribution of historical earthquakes and the GPS-derived horizontal velocity field we conclude that the Santorini–Amorgos zone is presently in the state of right-lateral transtension reflecting a major structural boundary of the volcanic arc subdividing it into a seismically and volcanically quiet western and an active eastern part." @default.
• W2067396832 created "2016-06-24" @default.
• W2067396832 creator A5004286121 @default.
• W2067396832 creator A5035695025 @default.
• W2067396832 creator A5039612979 @default.
• W2067396832 creator A5050542006 @default.
• W2067396832 creator A5078262885 @default.
• W2067396832 creator A5086997811 @default.
• W2067396832 date "2006-09-01" @default.
• W2067396832 modified "2023-10-11" @default.
• W2067396832 title "Microseismic activity in the Hellenic Volcanic Arc, Greece, with emphasis on the seismotectonic setting of the Santorini–Amorgos zone" @default.
• W2067396832 cites W1551395222 @default.
• W2067396832 cites W1913469372 @default.
• W2067396832 cites W1964373154 @default.
• W2067396832 cites W1976739497 @default.
• W2067396832 cites W1977216678 @default.
• W2067396832 cites W1984652754 @default.
• W2067396832 cites W1984719743 @default.
• W2067396832 cites W1987534722 @default.
• W2067396832 cites W1990276088 @default.
• W2067396832 cites W1992212136 @default.
• W2067396832 cites W1993041116 @default.
• W2067396832 cites W1995314866 @default.
• W2067396832 cites W2001008178 @default.
• W2067396832 cites W2004239639 @default.
• W2067396832 cites W2010879384 @default.
• W2067396832 cites W2014449029 @default.
• W2067396832 cites W2015739117 @default.
• W2067396832 cites W2027837756 @default.
• W2067396832 cites W2028673197 @default.
• W2067396832 cites W2033887723 @default.
• W2067396832 cites W2038213437 @default.
• W2067396832 cites W2041251745 @default.
• W2067396832 cites W2046685834 @default.
• W2067396832 cites W2054336508 @default.
• W2067396832 cites W2057569235 @default.
• W2067396832 cites W2058785554 @default.
• W2067396832 cites W2060610959 @default.
• W2067396832 cites W2063332136 @default.
• W2067396832 cites W2065204617 @default.
• W2067396832 cites W2071786173 @default.
• W2067396832 cites W2073789854 @default.
• W2067396832 cites W2080313786 @default.
• W2067396832 cites W2080750169 @default.
• W2067396832 cites W2083682447 @default.
• W2067396832 cites W2084724762 @default.
• W2067396832 cites W2090215278 @default.
• W2067396832 cites W2093378882 @default.
• W2067396832 cites W2099857446 @default.
• W2067396832 cites W2102790268 @default.
• W2067396832 cites W2103429433 @default.
• W2067396832 cites W2106392680 @default.
• W2067396832 cites W2122562158 @default.
• W2067396832 cites W2134461822 @default.
• W2067396832 cites W2154259004 @default.
• W2067396832 cites W2169944521 @default.
• W2067396832 cites W2171596042 @default.
• W2067396832 cites W2174857550 @default.
• W2067396832 cites W4234701869 @default.
• W2067396832 cites W4250705285 @default.
• W2067396832 doi "https://doi.org/10.1016/j.tecto.2006.03.024" @default.
• W2067396832 hasPublicationYear "2006" @default.
• W2067396832 type Work @default.
• W2067396832 sameAs 2067396832 @default.
• W2067396832 citedByCount "94" @default.
• W2067396832 countsByYear W20673968322012 @default.
• W2067396832 countsByYear W20673968322013 @default.
• W2067396832 countsByYear W20673968322014 @default.
• W2067396832 countsByYear W20673968322015 @default.
• W2067396832 countsByYear W20673968322016 @default.
• W2067396832 countsByYear W20673968322017 @default.
• W2067396832 countsByYear W20673968322018 @default.
• W2067396832 countsByYear W20673968322019 @default.
• W2067396832 countsByYear W20673968322020 @default.
• W2067396832 countsByYear W20673968322021 @default.
• W2067396832 countsByYear W20673968322022 @default.
• W2067396832 countsByYear W20673968322023 @default.
• W2067396832 crossrefType "journal-article" @default.
• W2067396832 hasAuthorship W2067396832A5004286121 @default.
• W2067396832 hasAuthorship W2067396832A5035695025 @default.
• W2067396832 hasAuthorship W2067396832A5039612979 @default.
• W2067396832 hasAuthorship W2067396832A5050542006 @default.
• W2067396832 hasAuthorship W2067396832A5078262885 @default.
• W2067396832 hasAuthorship W2067396832A5086997811 @default.
• W2067396832 hasBestOaLocation W20673968322 @default.
• W2067396832 hasConcept C120806208 @default.
• W2067396832 hasConcept C127313418 @default.
• W2067396832 hasConcept C165205528 @default.
• W2067396832 hasConcept C183222429 @default.
• W2067396832 hasConcept C58097730 @default.
• W2067396832 hasConcept C7266685 @default.
• W2067396832 hasConcept C77928131 @default.
• W2067396832 hasConcept C83176761 @default.
• W2067396832 hasConceptScore W2067396832C120806208 @default.
• W2067396832 hasConceptScore W2067396832C127313418 @default.
• W2067396832 hasConceptScore W2067396832C165205528 @default.
• W2067396832 hasConceptScore W2067396832C183222429 @default.
• W2067396832 hasConceptScore W2067396832C58097730 @default.

• next