Search results for "Geophysic"

showing 10 items of 2684 documents

Geochemical and Petrographic Characterization of Marine-Continental Transitional Facies Shale (Qilian Basin, China): Origin of Organic Matter Input, …

2021

This study, for the first time, investigates the source, keroger pattern, evolution degree, sedimentary environment, and evaluates the hydrocarbon generating ability of marine-continental transitional facies shale from the Ebao area of the Qilian Basin in western China. The organic-rich shales of the marine-continental transitional facies were subjected to total organic carbon (TOC), rock pyrolysis, the biomarkers and kerogen microscopy analyses. The kerogen microscopy analyses indicated that the sample from ZK001 well and ZK2002 well had a mass of vitrinite and small number of exinite, so kerogen type was mainly humic. According to vitrinite reflectance, the organic matter was in the stage…

Science0211 other engineering and technologiesGeochemistry02 engineering and technologyshales010502 geochemistry & geophysics01 natural sciencesPetrographySedimentary depositional environmentchemistry.chemical_compoundKerogenmarine-continental transitional faciesOrganic matter021108 energyVitrinite0105 earth and related environmental scienceschemistry.chemical_classificationMaturity (geology)QQilian BasinbiomarkerschemistryFaciesGeneral Earth and Planetary SciencesOil shaleGeologyhydrocarbon-generating potentialFrontiers in Earth Science
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Submerged speleothems and sea level reconstructions: a global overview and new results from the Mediterranean Sea

2021

This study presents a global overview of the submerged speleothems used to reconstruct paleo sea levels and reports new results from two stalactites collected in the Mediterranean Sea. Coastal cave deposits significantly contributed to the understanding of global and regional sea-level variations during the Middle and Late Quaternary. The studied speleothems cover the last 1.4 Myr and focused mainly on Marine Isotope Stages (MIS) 1, 2, 3, 5.1, 5.3, 5.5, 7.1, 7.2, 7.3 and 7.5. The results indicate that submerged speleothems represent extraordinary archives that can provide detailed information on former sea-level changes. The two stalactites collected in the central Mediterranean Sea, at Fa…

Sea level change010506 paleontologyStalactitevertical tectonic movementGeography Planning and DevelopmentAquatic Science010502 geochemistry & geophysics01 natural sciencesBiochemistryMediterranean seaCaveSea-level changeSea cave14. Life underwaterTD201-500Sea levelPhreatic[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/OceanographySea caves0105 earth and related environmental sciencesWater Science and Technology[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesPhreatic speleothemHydraulic engineeringFavignana; Phreatic speleothem; Sea caves; Sea-level change; Submerged speleothem; Ustica; Vertical tectonic movementsFavignanaOceanographyUsticaQuaternaryFavignana Phreatic speleothem Sea caves Sea-level change Submerged speleothem Ustica Vertical tectonic movementsTC1-978Submerged speleothemVertical tectonic movementsGeology
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An improvement of June-September rainfall forecasting in the Sahel based upon region April-May moist static energy content (1968-1997)

1999

This study provides statistical evidence that June–September Sahelian rainfall hindcasts currently based on oceanic thermal predictors apprehend more the negative trend than the interannual rainfall variations. Four physically meaningful predictors of June–September Sahel rainfall are first selected through the near-surface April–May information and several experimental hindcasts provided. We then discuss the skills achieved using regression techniques and cross-validated discriminant functions. In that context, 8/11 of the driest seasons and 8/10 of the wettest are correctly predicted. Finally using completely independent training and working periods we show that better and significant hin…

Sea surface temperatureGeophysicsClimatologyTraining (meteorology)Moist static energyGeneral Earth and Planetary SciencesHindcastForecast skillEnvironmental scienceContext (language use)Regression analysisStatistical evidenceGeophysical Research Letters
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Litter contribution to soil organic carbon in the processes of agriculture abandon

2015

The mechanisms of litter decomposition, translocation and stabilization into soil layers are fundamental processes in the functioning of the ecosystem, as they regulate the cycle of soil organic matter (SOM) and CO2 emission into the atmosphere. In this study the contribution of litters of different stages of Mediterranean secondary succession on carbon sequestration was investigated, analyzing the role of earthworms in the translocation of SOM into the soil profile. For this purpose the δ13C difference between meadow C4-C soil and C3-C litter was used in a field experiment. Four undisturbed litters of different stages of succession (45, 70, 100 and 120 since agriculture abandon) were colle…

Secondary successionSettore AGR/05 - Assestamento Forestale E SelvicolturaStratigraphySoil biologySoil ScienceCarbon sequestrationlcsh:StratigraphyGeochemistry and PetrologySoil Science; Earth-Surface Processes; Geochemistry and Petrology; Geology; Geophysics; Paleontology; StratigraphyGeophysiclcsh:QE640-699Earth-Surface ProcessesEcologySoil organic matterlcsh:QE1-996.5PaleontologyGeologySoil carbonPlant litterSettore AGR/02 - Agronomia E Coltivazioni Erbaceelcsh:GeologyGeophysicsAgronomyEarth-Surface ProcesseSoil waterEnvironmental scienceSoil horizon
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Mineralogical and chemical variability of fluvial sediments: 1. Bedload sand (Ganga–Brahmaputra, Bangladesh)

2010

This study investigates the natural processes that control concentration of detrital minerals and consequently chemical elements in river sand. The novelty of our approach consists in the systematic integration of detailed textural, petrographical, mineralogical and chemical data, and in the quantitative description and modeling of relationships among mineralogical and chemical variables for each sample and each grain-size class in each sample. Bed sediment in transit in the largest sedimentary system on Earth chiefly consists of fine-grained lithofeldspatho quartzose sand including rich amphibole–epidote–garnet suites, mixed with minor very-fine grained-sand to silt subpopulations containi…

Sedimentary petrologyProvenanceHimalayaGeochemistrysedimentary geochemistry sedimentary petrology settling equivalence selective entrainment placer sands opaque minerals REE-bearing minerals Eu anomaly HimalayaSedimentFluvialEu anomalyWeatheringSiltSedimentary geochemistryGeophysicsPlacer sandSettling equivalenceSpace and Planetary ScienceGeochemistry and PetrologyOpaque mineralEarth and Planetary Sciences (miscellaneous)Sedimentary rockGEO/02 - GEOLOGIA STRATIGRAFICA E SEDIMENTOLOGICAREE-bearing mineralSelective entrainmentChemical compositionGeologyBed load
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Inferring rheology and geometry of subsurface structures by adjoint-based inversion of principal stress directions

2020

SUMMARY Imaging subsurface structures, such as salt domes, magma reservoirs or subducting plates, is a major challenge in geophysics. Seismic imaging methods are, so far, the most precise methods to open a window into the Earth. However, the methods may not yield the exact depth or size of the imaged feature and may become distorted by phenomena such as seismic anisotropy, fluid flow, or compositional variations. A useful complementary method is therefore to simulate the mechanical behaviour of rocks on large timescales, and compare model predictions with observations. Recent studies have used the (non-linear) Stokes equations and geometries from seismic studies in combination with an adjoi…

Seismic anisotropy010504 meteorology & atmospheric sciencesDiscretizationGeophysical imagingObservableGeometry010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsNonlinear systemGeophysicsRheologyGeochemistry and Petrology13. Climate actionFluid dynamicsGeology0105 earth and related environmental sciencesSalt domeGeophysical Journal International
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Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone …

2021

Abstract Detecting the presence and geometry of crustal shear zones by geophysical methods relies on our understanding of the intrinsic parameters controlling the seismic properties of these deformed rocks, over the range of pressure-temperature conditions expected in the Earth's crust. To this end, we aimed to track changes in P-wave propagation velocity (VP), anisotropy (AVP) and S-wave splitting (AVS) across a natural shear zone using experimental and electron backscatter diffraction methods. Five samples were collected across a meter-scale shear zone developed under amphibolite- to greenschist-facies in the Neves metagranodiorite (Tauern Window, Eastern Alps). With increasing strain, se…

Seismic anisotropyDeformation (mechanics)GreenschistCrustengineering.materialPhysics::GeophysicsLineationGeophysicsengineeringPlagioclaseShear zonePetrologyAnisotropyGeologyEarth-Surface ProcessesTectonophysics
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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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