Search results for "GEODYNAMICS"

showing 10 items of 32 documents

Tertiary Ultrapotassic Volcanism in Serbia: Constraints on Petrogenesis and Mantle Source Characteristics

2005

The Serbian province of Tertiary ultrapotassic volcanism is related to a post-collisional tectonic regime that followed the closure of the Tethyan Vardar Ocean by Late Cretaceous subduction beneath the southern European continental margin. Rocks of this province form two ultrapotassic groups; one with affinities to lamproites, which is concentrated mostly in the central parts of the Vardar ophiolitic suture zone, and the other with affinities to kamafugites, which crops out in volcanoes restricted to the western part of Serbia. The lamproitic group is characterized by a wide range of Sr/Sri (0 70735–0 71299) and Nd/Ndi (0 51251–0 51216), whereas the kamafugitic group is isotopically more ho…

Peridotite010504 meteorology & atmospheric sciencesGeochemistryPartial melting550 - Earth sciencesengineering.materialGeodynamics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geophysics13. Climate actionGeochemistry and PetrologyUltramafic rockengineeringPhlogopiteMetasomatismGeology0105 earth and related environmental sciencesPetrogenesisJournal of Petrology
researchProduct

A network of superconducting gravimeters as a detector of matter with feeble nongravitational coupling

2020

Abstract Hidden matter that interacts only gravitationally would oscillate at characteristic frequencies when trapped inside of Earth. For small oscillations near the center of the Earth, these frequencies are around 300 μHz. Additionally, signatures at higher harmonics would appear because of the non-uniformity of Earth’s density. In this work, we use data from a global network of gravimeters of the International Geodynamics and Earth Tide Service (IGETS) to look for these hypothetical trapped objects. We find no evidence for such objects with masses on the order of 1014 kg or greater with an oscillation amplitude of 0.1 re. It may be possible to improve the sensitivity of the search by s…

Physics010308 nuclear & particles physicsGravimeter530 PhysicsInner coreAstronomyEarth tideGeodynamics530 Physik01 natural sciencesAtomic and Molecular Physics and OpticsPhysics::GeophysicsCoupling (physics)Orders of magnitude (time)HarmonicsPhysics::Space Physics0103 physical sciencesAstrophysics::Earth and Planetary Astrophysics010306 general physicsNoise (radio)
researchProduct

Modeling evolution of the San Andreas Fault system in northern and central California

2012

[1] We present a three-dimensional finite element thermomechanical model idealizing the complex deformation processes associated with evolution of the San Andreas Fault system (SAFS) in northern and central California over the past 20 Myr. More specifically, we investigate the mechanisms responsible for the eastward (landward) migrationof the San Andreas plate boundary over time, a process thathas largely determined the evolution and present structure of SAFS. Two possible mechanisms had been previously suggested. One mechanism suggests that the Pacific plate first cools and captures uprising mantle in the slab window, subsequently causing accretion of the continental crustal blocks. An alt…

Plate tectonicsGeophysicsSubductionGeochemistry and PetrologyPacific PlateSlab windowCrustGeophysicsPresent dayGeodynamicsSeismologyMantle (geology)GeologyGeochemistry, Geophysics, Geosystems
researchProduct

Deriving scaling laws in geodynamics using adjoint gradients

2018

Abstract Whereas significant progress has been made in modelling of lithospheric and crustal scale processes in recent years, it often remains a challenge to understand which of the many model parameters is of key importance for a particular simulation. Determining this is usually done by manually changing the model input parameters and performing new simulations. For a few cases, such as for folding or Rayleigh-Taylor instabilities, one can use thick-plate stability analysis to derive scaling laws to obtain such insights. Yet, for more general cases, it is not straightforward to do this (apart from running many simulations). Here, we discuss a numerically cheaper approach to compute scalin…

Scaling law010504 meteorology & atmospheric sciencesScale (ratio)Folding (DSP implementation)Geodynamics010502 geochemistry & geophysics01 natural sciencesInstabilityStability (probability)Theoretical physicsGeophysicsKey (cryptography)Statistical physicsGeologySingle layer0105 earth and related environmental sciencesEarth-Surface ProcessesTectonophysics
researchProduct

Crustal Structure of the Seismogenic Volume of the 2010–2014 Pollino (Italy) Seismic Sequence From 3D P- and S-Wave Tomographic Images

2021

A tomographic analysis of Mt. Pollino area (Italy) has been performed using earthquakes recorded in the area during an intense seismic sequence that occurred between 2010 and 2014. 870 local earthquakes with magnitude ranging from 1.8 to 5.0 were selected considering the number of recording stations, the signal quality, and the hypocenter distribution. P- and S-wave arrival times were manually picked and used to compute 3D velocity models through tomographic seismic inversion. The resulting 3D distributions of VP and VS are characterized by high resolution in the central part of the investigated area and from surface to about 10 km below sea level. The aim of the work is to obtain high-qual…

Seismic gapHypocenterseismic gapScienceQseismic sequenceMagnetic dipMagnitude (mathematics)Context (language use)Induced seismicitycrustal structurePollinoTectonicsgeodynamics and seismicitycrustal structure; geodynamics and seismicity; Italian Apennine; Pollino; seismic gap; seismic sequence; velocity tomographyGeneral Earth and Planetary SciencesSeismic inversionItalian Apenninevelocity tomographySeismologyGeologyFrontiers in Earth Science
researchProduct

Use of CORS Time Series for Geodynamics Applications in Western Sicily (Italy)

2020

In the last few decades, the use of GNSS Continuously Operating Reference Station (CORS) networks allowed improving the accuracy of real-time positioning and post-processing positioning. In this way, several applications have been performed including remote sensing, agriculture, cultural heritage and geodynamics studies. The latter have been developed analysing CORS time-series and consistent data over long periods were needed to validate the results. In Italy, specifically in Sicily, two CORS networks were be used to monitor the geodynamics motions: the Istituto Nazionale di Geofisica e Vulcanologia (INGV) GNSS CORS network in the eastern part and the University of Palermo (UNIPA) GNSS COR…

Series (stratigraphy)GNSS applicationsRemote sensing (archaeology)GeodynamicsPrecise Point PositioningGeodesyCORS Geodynamic GNSS data PPP data Time seriesSettore ICAR/06 - Topografia E CartografiaGeologyLinear trend
researchProduct

Structural architecture and active deformation pattern in the northern sector of the Aeolian-Tindari-Letojanni fault system (SE Tyrrhenian Sea-NE Sic…

2017

Framed in the current geodynamics of the central Mediterranean, the Aeolian-Tindari-Letojanni fault system is part of a wider NW-SE oriented right-lateral wrench zone which accommodates diverging motion between regional-scale blocks located at the southern edge of the Calabrian Arc. In order to investigate the structural architecture and the active deformation pattern of the northern sector of this tectonic feature, structural observations on-land, high and very-high resolution seismic reflection data, swath bathymetry data and seismological and geodetic data were merged from the Lipari-Vulcano volcanic complex (central sector of the Aeolian Islands) to the Peloritani Mountains across the G…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesSettore GEO/03 - Geologia StrutturaleStructural analysisGPS geodesyInduced seismicityFault (geology)010502 geochemistry & geophysics01 natural sciencesSouthern Tyrrhenian seaNE SicilySouthern Tyrrhenian sea NE Sicily seismic reflection profiles structural analysis seismology GPS geodesyBathymetrySeismology0105 earth and related environmental sciencesgeographySeismic reflection profilesgeography.geographical_feature_categoryGeodetic datumGeologyGeophysicsGeodynamicsTectonicsVolcanoMagmaGeneral Earth and Planetary SciencesSouthern Tyrrhenian sea NE Sicily seismic reflection profiles structural analysis seismology GPS geodesy.SeismologyGeologyItalian Journal of Geosciences
researchProduct

A possible bridge between Adria and Africa: New palaeobiogeographic and stratigraphic constraints on the Mesozoic palaeogeography of the Central Medi…

2010

Abstract Dinosaur records in central and southern Italy testify to the occurrence of a diverse dinosaur fauna on the Apennine and Apulian carbonate platforms at least from the Tithonian to the Santonian. Most of the palaeogeographic reconstructions show these domains as topographically isolated areas, separated by deep pelagic basins and far from emerged continental areas. Thus, they hardly justify the long-lasting occurrence of these terrestrial vertebrates. Recent studies on the Mesozoic Panormide Carbonate Platform (western Sicily) yielded important stratigraphical and palaeontological data, which provide evidence for a convincing explanation of this unresolved problem. The recent discov…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformFaunatethyspalaeogeographySubsidenceGeodynamicsPaleontologychemistry.chemical_compoundPanormide Carbonate Platform dinosaurs Mesozoic palaeogeography Tethys geodynamicschemistrymesozoicGeneral Earth and Planetary SciencesMediterranean areaCarbonatepanormide carbonate platformgeodynamicsMesozoicdinosaurs; geodynamics; mesozoic; palaeogeography; panormide carbonate platform; tethysdinosaursPalaeogeographyGeologyEarth-Science Reviews
researchProduct

INTRODUCING THE SIRIPRO PROJECT: THE SICILY GEODYNAMIC SETTING. STATE OF THE ART

2009

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSICILY GEODYNAMICSSEISMIC REFLECTIONSIRIPRO
researchProduct

Water and Geodynamics

2006

Hydrogen is the most abundant element (Fig. 1⇓) in the galaxy and our solar system (Lodders 2003). Therefore it is not astonishing that hydrogen is a key player in the geodynamic evolution of planets. Its fate in the early Earth, after condensation of the solar nebula, the accretion of our planet and hydrogen reprocessing through early asteroidal and cometary bombardment (Dauphas et al. 2000) and segregation of a proto-Earth into iron core and silicate mantle is described elsewhere in this volume (Marty and Yokochi 2006). Figure 1. Abundance of elements in the solar system in numbers of atoms per 106 atoms of silicon (Lodders 2003). This chapter concerns itself with the geodynamics of the m…

Solar SystemHydrogenchemistryGeochemistry and PetrologyPlanetchemistry.chemical_elementGeodynamicsFormation and evolution of the Solar SystemEarly EarthGeologyMantle (geology)Abundance of the chemical elementsAstrobiologyReviews in Mineralogy and Geochemistry
researchProduct