Search results for "Induced"

showing 10 items of 1287 documents

Radon measurements in the SE and NE flank of Mt. Etna (Italy)

2007

Abstract Soil Radon has been monitored at two fixed sites located in the northeastern and southeastern flank of Mt. Etna. In this study we report the comparison between in-soil Radon concentration trend recorded in the SE flank and that one recorded in the NE one, where an in-soil Radon detection system is operating since 2001. The aim of this work was to implement the investigation area finding a suitable radon detection site, in the south-east flank of Mt. Etna, in order to better understand possible links between Radon anomalies and volcano dynamic. Radon data collected in NE and SE sites were compared with the volcanic tremor, frequency of occurrence of earthquakes and seismic strain-re…

geographyFlankRadiationgeography.geographical_feature_categoryFrequency of occurrenceMt. Etnachemistry.chemical_elementRadonInduced seismicityPower spectrumVolcanochemistryRadonSettore GEO/11 - Geofisica ApplicataInstrumentationSeismologyGeology
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Recent Activity and Kinematics of the Bounding Faults of the Catanzaro Trough (Central Calabria, Italy): New Morphotectonic, Geodetic and Seismologic…

2021

A multidisciplinary work integrating structural, geodetic and seismological data was performed in the Catanzaro Trough (central Calabria, Italy) to define the seismotectonic setting of this area. The Catanzaro Trough is a structural depression transversal to the Calabrian Arc, lying in-between two longitudinal grabens: the Crati Basin to the north and the Mesima Basin to the south. The investigated area experienced some of the strongest historical earthquakes of Italy, whose seismogenic sources are still not well defined. We investigated and mapped the major WSW–ENE to WNW–ESE trending normal-oblique Lamezia-Catanzaro Fault System, bounding to the north the Catanzaro Trough. Morphotectonic …

geographyQE1-996.5geography.geographical_feature_categoryTrough (geology)Magnitude (mathematics)MorphotectonicsContext (language use)GeologyFault (geology)Induced seismicityFault scarpCalabrian ArcGrabeninstrumental seismicitymorphotectonicsGeneral Earth and Planetary Sciencesgeodetic dataGeologySeismologyGeosciences
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Passive vs. active degassing modes at an open-vent volcano (Stromboli, Italy)

2012

Abstract We report here on a UV-camera based field experiment performed on Stromboli volcano during 7 days in 2010 and 2011, aimed at obtaining the very first simultaneous assessment of all the different forms (passive and active) of SO 2 release from an open-vent volcano. Using the unprecedented spatial and temporal resolution of the UV camera, we obtained a 0.8 Hz record of the total SO 2 flux from Stromboli over a timeframe of ∼14 h, which ranged between 0.4 and 1.9 kg s −1 around a mean value of 0.7 kg s −1 and we concurrently derived SO 2 masses for more than 130 Strombolian explosions and 50 gas puffs. From this, we show erupted SO 2 masses have a variability of up to one order of mag…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMean valueFluxInduced seismicity010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyLong periodTemporal resolutionEarth and Planetary Sciences (miscellaneous)Infrared radiometervolcanic degassing Strombolian explosions puffing UV camera high time resolution SO2 fluxGeologySeismology0105 earth and related environmental sciencesEarth and Planetary Sciences Letters
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Tectonics and seismicity of the Tindari Fault System, southern Italy: Crustal deformations at the transition between ongoing contractional and extens…

2006

[1] The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional zone of brittle deformation located at the transition between ongoing contractional and extensional crustal compartments and lying above the western edge of a narrow subducting slab. Onshore structural data, an offshore seismic reflection profile, and earthquake data are analyzed to constrain the present geometry of the Tindari Fault System and its tectonic evolution since Neogene, including the present seismicity. Results show that this zone of deformation consists of a broad NNW trending system of faults including sets of right-lateral, left-lateral, and extensional faults as well as early strike-slip faults rewor…

geographygeography.geographical_feature_categoryContext (language use)Structural basinInduced seismicityFault (geology)NeogeneTectonicsGeophysicsGeochemistry and PetrologySlabSubmarine pipelineSeismologyGeologyTectonics
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An integrated approach to investigate the seismotectonics of northern Sicily and southern Tyrrhenian

2009

Abstract This paper deals with a comparison among recent structure and seismicity in the hinge zone between northern Sicily and southern Tyrrhenian, corresponding to both emerged and submerged northern portion of the Maghrebian chain. This hinge zone is part of a wider W–E trending right-lateral shear zone, mainly characterized by both a synthetic NW-SE/W–E oriented, and antithetic left-lateral N–S/NE-SW fault systems, which has been affecting the tectonic edifice, since the Pliocene. The inland structures have been mapped using aerial-photo interpretation, geological mapping and mesostructural analysis to reconstruct the stress regime in the study area. On the contrary, the offshore struct…

geographygeography.geographical_feature_categorySettore GEO/03 - Geologia StrutturaleSeismotectonicsStructural basinInduced seismicityFault (geology)Geologic mapTectonicsGeophysicsLithosphereShear zoneSeismologyGeologyNeotectonic Seismicity Seismotectonic Central Mediterranean Stress fieldEarth-Surface ProcessesTectonophysics
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The Problem of Volcanic Unrest: The Campi Flegrei Case History

1996

Campi Flegrei is one of the most densely populated active volcanic areas of the world. It consists of a complex structure with a multicollapse caldera and many postcaldera, explosive, mostly monogenetic vents. The last eruption was in 1538 (Mt. Nuovo). Progressive reduction of eruption energy has accompanied migration of the vents toward the center of the caldera. Campi Flegrei activity is fed by a shallow magma chamber in which trachybasaltic magma undergoes cooling and fractionation, producing trachytic residual melt that is periodically tapped and erupted to the surface. The depth of the chamber is estimated, from petrological and active and passive seismic data, to be about 4 km beneath…

geographygeography.geographical_feature_categoryVolcanoMagmaCalderaTrachyteMagma chamberInduced seismicityUnrestSeismologyFumarole
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Flow changes and geochemical anomalies in warm and cold springs associated with the 1992-1994 seismic sequence at Pollina, Central Sicily, Italy

2007

During a three-year discontinuous geochemical monitoring of some warm springs and cold discharges located in central-northern Sicily, some hydro-geochemical changes were observed. Excluding a possible related to a moderate seismic activity were accidentally identified. The observed anomalies showed amplitudes that were modulated by the different geometries and volumes of the feeding aquifers. A poroelastic aquifer contraction, a shaking-induced dilatancy theory as well as seismogenetic-induced changes in the properties of the aquifers have been proposed as possible mechanisms for the water flow and hydro-geochemical changes. These preliminary results could be used to design a monitoring net…

geographygeography.geographical_feature_categoryWater flowEarthquake predictionAquiferInduced seismicityCrustal stressGeophysicsGeochemistry and PetrologyPetrologyGroundwaterGeologySeismologyEarthquake Prediction Flow Change Geochemical Parameter Geochemical Anomaly Crustal Stress
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Activation of Grapevine Defense Mechanisms: Theoretical and Applied Approaches

2011

part 4.; International audience; Grapevine, as other plants, possesses an innate immune system that usually prevents infection by pathogens. General elicitors are compounds of different biochemical families capable of inducing plant defense reactions. In grapevine, the cascade of defense events induced by elicitors has been studied among others in cell suspensions. The perception of the elicitor triggers signaling events that allow the activation of defense genes encoding PR proteins and other proteins involved in phytoalexin production and cell wall reinforcement. The grapevine phytoalexins resveratrol and derivated compounds have been largely studied. In addition to their antimicrobial ac…

grapevine defence réactions induced résistance elicitors0106 biological scienceschemistry.chemical_classification0303 health sciencesInnate immune system[SDV]Life Sciences [q-bio]PhytoalexinDefence mechanismsfood and beveragesBiologyResveratrol01 natural sciencesCell biologyElicitorCell wall03 medical and health scienceschemistry.chemical_compoundchemistry[SDE]Environmental SciencesPlant defense against herbivoryLimited disease030304 developmental biology010606 plant biology & botany
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Minimum detection limits and applications of proton and helium induced X-ray emission using transition-edge sensor array

2017

Abstract We have determined minimum detection limits, MDLs, for elements 14 ⩽ Z ⩽ 86 using a transition-edge sensor array, TES array, and as a comparison using an Amptek X-123SDD silicon drift detector, SDD. This was done using a 3 MeV proton beam and a 5.1 MeV helium beam. MDLs were determined for a thin film sample on top of C substrate, and for a bulk sample containing mostly Al. Due to the higher peak-to-background ratio, lower detection limits were obtainable using the TES array for most of the elements. However, for elements 30 ⩽ Z ⩽ 45 the performance of the TES array was not as good as the SDD performance. This is due to the limitations of the TES used at energies >10 keV. The great…

helium-induced x-ray emissionNuclear and High Energy PhysicsSilicon drift detectorProtonAnalytical chemistrychemistry.chemical_element02 engineering and technologySubstrate (electronics)01 natural sciencesSensor array0103 physical sciencesPIXEThin film010306 general physicsInstrumentationHeliumPhysicsta114minimum detection limit021001 nanoscience & nanotechnologychemistryTransition edge sensor0210 nano-technologyTESBeam (structure)
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Data from: Symbiotic polydnavirus and venom reveal parasitoid to its hyperparasitoids

2018

Symbiotic relationships may provide organisms with key innovations that aid in the establishment of new niches. For example, during oviposition, some species of parasitoid wasps, whose larvae develop inside the bodies of other insects, inject polydnaviruses into their hosts. These symbiotic viruses disrupt host immune responses, allowing the parasitoid’s progeny to survive. Here, we show that symbiotic polydnaviruses also have a downside to the parasitoid’s progeny by initiating a multi-trophic chain of interactions that reveals the parasitoid larvae to their enemies. These enemies are hyperparasitoids that use the parasitoid progeny as host for their own offspring. We found that the virus …

herbivore salivafungiLife Sciencesmultitrophic interactionsPieris brassicaeherbivore-induced plant volatilesparasitic waspPE&RCLaboratorium voor EntomologieLysibia nanaBiosystematiekmedicine and health careBiosystematicsMedicineBrassica oleraceaEPSLaboratory of EntomologyCotesia glomerataplant-mediated interaction network
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