Search results for "Gravity anomaly"

showing 10 items of 10 documents

The marine activities performed within the TOMO-ETNA experiment

2016

<p>The TOMO-ETNA experiment was planned in order to obtain a detailed geological and structural model of the continental and oceanic crust beneath Mt. Etna volcano and northeastern Sicily up to the Aeolian Islands (southern Italy), by integrating data from active and passive refraction and reflection seismic methodologies, magnetic and gravity surveys. This paper focuses on the marine activities performed within the experiment, which have been carried out in the Ionian and Tyrrhenian Seas, during three multidisciplinary oceanographic cruises, involving three research vessels (“Sarmiento de Gamboa”, “Galatea” and “Aegaeo”) belonging to different countries and institutions. During the o…

0301 basic medicineSeismometerlcsh:QC851-999010502 geochemistry & geophysicsRemotely operated vehicle01 natural sciencesSonarGravity anomalyEtna offshore; Ionian and Tyrrhenian Seas; Marine geophysical data acquisition; Scientific cruise report; Geophysics03 medical and health sciencesSeismic refraction0105 earth and related environmental sciencesMarine geophysical data acquisitionIonian and Tyrrhenian Seaslcsh:QC801-809Ionian and Tyrrhenian SeaSeafloor spreadinglcsh:Geophysics. Cosmic physics030104 developmental biologyGeophysicsSeismic tomographyScientific cruise reportEtna offshorelcsh:Meteorology. ClimatologySubmarine pipelineGeologySeismologyAnnals of Geophysics
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A Multiphysics Approach to Constrain the Dynamics of the Altiplano‐Puna Magmatic System

2021

Continuous Interferometric Synthetic Aperture Radar (InSAR) monitoring (> 25 years) has revealed a concentric surface deformation pattern above the Altiplano-Puna magma body (APMB) in the central Andes. Here, we use a joint interpretation of seismic imaging, gravity anomalies and InSAR data to constrain location, 3D geometry and density of the magma body. By combining gravity modelling, thermomechanical modelling, scaling law analysis and Bayesian inference, we are able to create a relationship between the geometry of a mid-crustal magma body and surface observations. Furthermore, we can estimate the uncertainties associated with the geometry of the APMB and identify the most important para…

Buoyancy010504 meteorology & atmospheric sciencesGeophysical imagingMultiphysicsGeophysicsengineering.material010502 geochemistry & geophysics01 natural sciencesGravity anomalyGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyInterferometric synthetic aperture radarMagmaEarth and Planetary Sciences (miscellaneous)engineeringDensity contrastJoint (geology)Geology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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Constraining effective rheology through parallel joint geodynamic inversion

2014

Abstract The dynamics of crust and lithosphere is to a large extent controlled by its effective viscosity. Unfortunately, extrapolation of laboratory experiments indicates that viscosity is likely to vary over many orders of magnitude. Additional methods are thus required to constrain the effective viscosity of the present-day lithosphere using more direct geophysical observations. Here we discuss a method, which couples 3D geodynamic models with observations (surface velocities and gravity anomalies) and with a Bayesian inversion scheme on massively parallel high performance computers. We illustrate that the basic principle of a joint geodynamic and gravity inversion works well with a simp…

ExtrapolationInversion (meteorology)CrustGeophysicsGeodynamicsParameter spaceGravity anomalyPhysics::GeophysicsGeophysics13. Climate actionLithosphereTectonophysicsGeologyEarth-Surface ProcessesTectonophysics
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Gravity Anomalies Over The Gongola Arm, Upper Benue Trough, Nigeria

2005

A regional gravity survey of the Gongola Arm of the Benue trough was carried out with the aim of determining structures of interest. The results of the gravity interpretation showed that the area of study is characterized by negative Bouguer anomalies that trend in the NE-SW direction and range in value from -75 to -15 mGal with an average of -42 mGal. A first order polynomial was used to approximate the regional anomalies in the area. The residual gravity anomaly map shows anomalies that range in value from -32 to +20 mGal. 2.5-D modeling of the residual gravity anomalies suggests that the area has a horst and graben structure, with the grabens being as large as 60 km in width and filled w…

GrabenGravity (chemistry)Horst and grabenHalf-grabenTrough (geology)First orderSeismologyGravity anomalyGeologyGlobal Journal of Geological Sciences
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Fundamentals of Gravity, Elements of Potential Theory

2009

PhysicsTheoretical physicsGravity (chemistry)Classical mechanicsMass elementHarmonic functionGravity effectGravity anomalyPotential theory
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Gravity Anomalies and Disturbances: Reductions and Analyses

2009

Reference ellipsoidGeodesyGeologyBouguer anomalyGravity anomaly
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Sicily’s fold–thrust belt and slab roll-back: the SI.RI.PRO. seismic crustal transect

2016

Sicily is a thick orogenic wedge formed by (1) the foreland (African) and its Sicilian orogen and (2) the thick-skinned, Calabrian–Peloritani wedge. The crust under central Sicily, from the Tyrrhenian margin to the coastline of the Sicily Channel, has been investigated by the multidisciplinary (SI.RI.PRO.) research project. The project dealt with the nature and thickness of the crust and depth and geometry of the Moho, which is essential in formulating subduction models and improving the knowledge of African and Tyrrhenian–European lithospheres. The results resolve features such as (1) the main orogenic wedge, (2) the very steep, NW–SE-trending regional monocline suggesting inflection of th…

SubductionSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGeologyCrustFold (geology)language.human_languageGravity anomalycrustal structureBasement (geology)MonoclineSettore GEO/11 - Geofisica Applicatalanguageseismic reflectionPetrologySicilianForeland basinsubductionGeologySeismology
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Seasonal and Inter-annual Variation of Evapotranspiration in Amazonia Based on Precipitation, River Discharge and Gravity Anomaly Data

2019

We analyzed seasonal and spatial variations of evapotranspiration (ET) for five Amazon sub-basins and their response to the 2015/16 El Nino episode using a recently developed water-budget approach. ET varied typically between similar to 7 and 10 cm/month with exception of the Xingu basin for which it varied between 10 and 15 cm/month. Outstanding features of ET seasonality are (i) generally weak seasonality, (ii) two ET peaks for the two very wet catchments Solimoes and Negro, with one occurring during the wet season and one during the drier season, and (iii) a steady increase of ET during the second half of the dry season for the three drier catchments (Madeira, Tapajos, Xingu). Peak ET oc…

Wet season1171 Geosciences010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGravity anomalyCARBONSolar induced fluorescenceAmazoniaGRACEEvapotranspirationDry seasonmedicinePrecipitationEl NiñoFLUORESCENCElcsh:ScienceSATELLITE0105 earth and related environmental sciencesBASINForest ProductivityEvapotranspirationAmazon rainforestDischargePHOTOSYNTHESISSENSORRAIN-FOREST15. Life on landSeasonalitymedicine.diseaseBRAZILVARIABILITY13. Climate actionGeneral Earth and Planetary SciencesEnvironmental sciencelcsh:QEl Nino
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Crustal structures of the Sicily orogene along the SIRIPRO seismic profile

2012

crustal multichannel seismic profile gravity anomaly sicilian fold and thrust beltSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale
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Inversion of gravity anomalies over spreading oceanic ridges

2005

Abstract Models of spreading ocean ridges are derived by Bayesian gravity inversion with geophysical and geodynamic a priori information. The aim is to investigate the influence of spreading rate, plate dynamics and tectonic framework on crust and upper mantle structure by comparing the Mid Atlantic Ridge (MAR), the Indian Ocean Ridge (IND) and the East Pacific Rise (PAC). They differ in mean spreading rate, dynamic settings, as attached slabs, and plume interaction. Topography or bathymetry, gravity, isostasy, seismology and geology, etc. are averaged along the ridges and guide the construction of initial 2D models, including features as mean plumes, i.e. averaged along the ridge. This is …

geographygeography.geographical_feature_categorySlab pullMid-ocean ridgeGeophysicsMid-Atlantic RidgeGravity anomalySeafloor spreadingGeophysicsRidge pushRidgeLithosphereGeologyEarth-Surface ProcessesJournal of Geodynamics
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