Search results for "feature"

showing 10 items of 4091 documents

Impact of storms on mixed carbonate and siliciclastic shelves: insights from combined diffusive and fluid-flow transport stratigraphic forward model

2004

Abstract A quantitative stratigraphic model of mixed carbonate/siliciclastic continental shelves is presented to investigate the relationships between depositional processes and stratigraphic responses at long‐term, large spatial scales. A diffusion model is combined with a fluid‐flow approach to simulate both long‐term factors, i.e. the processes controlling large‐scale architecture, and short‐term processes, i.e. sediment redistribution by storms. Any net sediment accumulation is the result of the succession of a storm and a fair‐weather period. Sediments are mobilized by waves and advected by low‐frequency currents during storm events. Sediments are then reworked and redistributed downsl…

Sedimentary depositional environmentgeographygeography.geographical_feature_categoryContinental shelfAdvectionSedimentGeologySiliciclasticStormSediment transportGeomorphologyGeologyGeobiologyBasin Research
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Automatic Segmentation Using a Hybrid Dense Network Integrated With an 3D-Atrous Spatial Pyramid Pooling Module for Computed Tomography (CT) Imaging

2020

Computed tomography (CT) with a contrast-enhanced imaging technique is extensively proposed for the assessment and segmentation of multiple organs, especially organs at risk. It is an important factor involved in the decision making in clinical applications. Automatic segmentation and extraction of abdominal organs, such as thoracic organs at risk, from CT images are challenging tasks due to the low contrast of pixel values surrounding other organs. Various deep learning models based on 2D and 3D convolutional neural networks have been proposed for the segmentation of medical images because of their automatic feature extraction capability based on large labeled datasets. In this paper, we p…

SegTHOR0209 industrial biotechnologyGeneral Computer ScienceComputer scienceFeature extractionComputingMethodologies_IMAGEPROCESSINGANDCOMPUTERVISION02 engineering and technologyConvolutional neural network020901 industrial engineering & automationPyramid0202 electrical engineering electronic engineering information engineeringMedical imagingGeneral Materials ScienceSegmentationPyramid (image processing)3D deep learning modelsPixelbusiness.industryDeep learningGeneral EngineeringPattern recognition3D-atrous spatial pyramid pooling (ASPP)Feature (computer vision)3D volumetric segmentation020201 artificial intelligence & image processinglcsh:Electrical engineering. Electronics. Nuclear engineeringArtificial intelligencebusinesslcsh:TK1-9971IEEE Access
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Modeling Transit Flow Through Port Gates and Connecting Channel in Baltic Sea—Liepaja Port—Liepaja Lake System

2021

This study investigates a water transport features by extending Copernicus Marine Environment Service (CMEMS) to the Liepaja coast-port-channel-lake system with a two-way nested model. The Liepaja lake and Liepaja port are connected by Trade channel. The Liepaja port has three gates—the openings in wave breakers connecting the port aquatory with the Baltic sea. Each of gates has a corresponding dredged channel for securing the navigation. A hydrodynamic model is set up to study the flow and water level in this system. The area of the port gates, port and Trade channel are resolved by 33 m grid. The model results are verified against currents and sea level observations inside/outside port, T…

Seiche010504 meteorology & atmospheric sciencesScienceOcean EngineeringQH1-199.5Aquatic ScienceOceanography01 natural sciencestransit currents in portsport hydrodynamicsport seichesUnderwatertwo-way nesting0105 earth and related environmental sciencesWater Science and TechnologygeographyGlobal and Planetary ChangeWater transportgeography.geographical_feature_category010505 oceanographyQFetchOcean currentGeneral. Including nature conservation geographical distributionPort (computer networking)Water levelOceanographycoastal modelingGeologyChannel (geography)Frontiers in Marine Science
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Seismic anisotropy and its impact on imaging the shallow Alpine Fault : an experimental and modeling perspective.

2020

The transpressional Alpine Fault in New Zealand has created a thick shear zone with associated highly anisotropic rocks. Low seismic velocity zones (LVZ) and high seismic reflectivity are recorded in the Alpine Fault Zone, but no study has explored the underlying physical rock parameters of the shallow crust that control these observations. Protomylonites are the volumetrically dominant lithology of the fault zone. Here we combine experimental measurements of P‐wave speeds with numerical models of elastic wave anisotropy of protomylonite samples to explore how the fault zone can be seismically imaged. Numerical models that account for the porosity‐free real samples' fabric elastic tensors f…

Seismic anisotropygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLithologyCrustFault (geology)01 natural sciencesSeismic waveGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Reflection (physics)Shear zoneAnisotropySeismologyGeology0105 earth and related environmental sciences
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New insights into seismic absorption imaging

2020

Abstract In recent years, attenuation has been used as a marker for source and dynamic Earth processes due to its higher sensitivity to small variations of lithospheric properties compared to seismic velocity. From seismic hazard analysis to oil and gas exploration and rock physics, many fields need a better reconstruction of energy absorption, a constituent of seismic attenuation generally considered a reliable marker of fluid saturation in space. Here, we propose absorption tomography (AT), a technique grounded on the principles of scattering tomography and Multiple Lapse Time Window Analysis. We benchmark its efficiency to image absorption in space by comparing its results with those obt…

Seismic attenuationDiffusion (acoustics)010504 meteorology & atmospheric sciencesPhysics and Astronomy (miscellaneous)Seismic attenuation; Scattering; Absorption; Tomography; DiffusionFault (geology)010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsCodaAbsorptionScatteringDiffusionAbsorption (electromagnetic radiation)Tomography0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryAttenuationAstronomy and AstrophysicsTectonicsGeophysicsSeismic hazardSpace and Planetary ScienceTomographySeismology
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Understanding seismic path biases and magmatic activity at Mount St Helens volcano before its 2004 eruption

2020

SUMMARY In volcanoes, topography, shallow heterogeneity and even shallow morphology can substantially modify seismic coda signals. Coda waves are an essential tool to monitor eruption dynamics and model volcanic structures jointly and independently from velocity anomalies: it is thus fundamental to test their spatial sensitivity to seismic path effects. Here, we apply the Multiple Lapse Time Window Analysis (MLTWA) to measure the relative importance of scattering attenuation vs absorption at Mount St Helens volcano before its 2004 eruption. The results show the characteristic dominance of scattering attenuation in volcanoes at lower frequencies (3–6 Hz), while absorption is the primary atte…

Seismic attenuationgeographySeismic tomographygeography.geographical_feature_categoryNorth America; Coda waves; Seismic attenuation; Seismic tomography; Volcano seismology; Wave scattering and diffraction010504 meteorology & atmospheric sciencesCoda wavesVolcano seismology010502 geochemistry & geophysics01 natural sciencesMountGeophysicsVolcanoGeochemistry and PetrologySeismic tomographyWave scattering and diffractionNorth AmericaPath (graph theory)Volcano seismologySeismologyGeology0105 earth and related environmental sciencesGeophysical Journal International
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Interaction between seismicity and deformation on different time scales in volcanic areas: Campi Flegrei and Stromboli

2019

We study oscillations recorded at Stromboli and Campi Flegrei by different sensors: seismometers, strainmeters and tiltmeters. We examine both the high-frequency (>0.5 Hz) portion of the spectrum and very long period signals up to tidal scales. In this context, seismicity and deformation are investigated on different time scales (from minutes to days/years) in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. In this work, the strict relation of tides and volcanic processes is shown. At Stromboli, indeed the transition from the stationary phase to the non-stationary phase seems to have a tidal precu…

Seismometer010504 meteorology & atmospheric scienceslcsh:Dynamic and structural geologyanalysisfrequency analysisTiltmeterContext (language use)VolcanismInduced seismicity010502 geochemistry & geophysicsdiurnal variation01 natural sciencesvolcanic eruptionvolcanologylcsh:QE500-639.5lcsh:Science0105 earth and related environmental sciencesgeographyvolcanismgeography.geographical_feature_categoryVulcanian eruptionlcsh:QE1-996.5deformationGeneral MedicineVolcanologydeformation; diurnal variation; frequency analysis; numerical model; seismicity; time series; analysis; volcanic eruption; volcanism;volcanologylcsh:GeologyVolcanolcsh:Qseismicitytime seriesnumerical modelGeologySeismology
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Long term seismic noise acquisition and analysis in the Homestake Mine with tunable monolithic sensors

2009

In this paper we describe the scientific data recorded along one month of data taking of two mechanical monolithic horizontal sensor prototypes located in a blind-ended (side) tunnel 2000 ft deep in the Homestake (South Dakota, USA) mine chosen to host the Deep Underground Science and Engineering Laboratory (DUSEL). The two mechanical monolithic sensors, developed at the University of Salerno, are placed, in thermally insulating enclosures, onto concrete slabs connected to the bedrock, and behind a sound-proofing wall. The main goal of this experiment is to characterize the Homestake site in the frequency band 10-4 ÷ 30 H z and to estimate the level of Newtonian noise, providing also the ne…

SeismometerEngineeringgeographygeography.geographical_feature_categorybusiness.industryFrequency bandInstrumentationBedrockMineralogySeismic noiseTerm (time)Astronomical interferometerbusinessSeismologyNoise (radio)
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The INGV's new OBS/H: Analysis of the signals recorded at the Marsili submarine volcano

2009

Abstract The ocean bottom seismometer with hydrophone deployed on the flat top of the Marsili submarine volcano (790 m deep) by the Gibilmanna OBS Lab (CNT–INGV) from 12th to 21st July, 2006, recorded more than 1000 transient seismic signals. Nineteen of these signals were associated with tectonic earthquakes: 1 teleseismic, 8 regional (located by INGV) and 10 small local seismic events (non located earthquakes). The regional events were used to determine sensor orientation. By comparing the signals recorded with typical volcanic seismic activity, we were able to group all the other signals into three categories: 817 volcano–tectonic type B (VT-B) events, 159 occurrences of high frequency t…

Seismometergeographygeography.geographical_feature_categoryHydrophoneContinuous volcanic tremorFrequency bandPolarization analysiSpectral analysisMarsili SeamountTransient volcano–seismic signalSignalTectonicsGeophysicsVolcanoGeochemistry and PetrologyOBS/HTime domainSubmarine volcanoGeologySeismologyJournal of Volcanology and Geothermal Research
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Monochromatic Long-Period Seismicity Prior to the 2012 Earthquake Swarm at Little Sitkin Volcano, Alaska

2021

Detection of the earliest stages of unrest is one of the most challenging and yet critically needed aspects of volcano monitoring. We investigate a sequence of five unusual long-period (LP) earthquakes that occurred in the days prior to the onset of a months-long volcano-tectonic (VT) earthquake swarm beneath Little Sitkin volcano in the Aleutian Islands during late 2012. The long-period earthquakes had two distinctive characteristics: their signals were dominated by a monochromatic spectral peak at approximately 0.57 Hz and they had impulsive P and S-wave arrivals on a seismometer located on Amchitka Island 80 km to the southeast of the volcano. In each case, the monochromatic earthquakes …

Seismometerprecursory seismicitygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSciencevolcano seismologyQlong-period earthquakeInduced seismicity010502 geochemistry & geophysicsEarthquake swarm01 natural sciencesIntrusionearthquake swarmSillVolcanoresonanceLong periodGeneral Earth and Planetary SciencesMonochromatic colorSeismologyGeology0105 earth and related environmental sciencesFrontiers in Earth Science
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