Search results for "rock"

showing 10 items of 1160 documents

Thermobarometric constraints on pressure variations across the Plattengneiss shear zone of the Eastern Alps: implications for exhumation models durin…

2014

Forward and inverse mineral equilibria modelling of metapelitic rocks in the hangingwall and footwall of the Plattengneiss, a major shear zone in the Eastern Alps, is used to constrain their tectonometamorphic evolution and assess models for their exhumation. Forward (pseudosection) modelling of two metapelitic rocks suggests a steep clockwise P–T path with a near-isothermal decompression segment from a pressure peak at ~18–19 kbar and 670 °C to the metamorphic peak at 680–720 °C and 11–13 kbar. A subsequent decrease to 600–645 °C and 8–9 kbar is inferred from the late growth of staurolite in some samples. Conventional thermobarometric calculations (inverse modelling) on 18 samples with the…

SubductionMetamorphic rockGeologyGeochemistry and Petrologyvisual_artStauroliteSlabvisual_art.visual_art_mediumRelative pressureClockwiseShear zonePetrologyGeomorphologyGeologyPressure gradientJournal of Metamorphic Geology
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Porewater pressure control on subglacial soft sediment remobilization and tunnel valley formation: A case study from the Alnif tunnel valley (Morocco)

2014

25 pages; International audience; In the eastern part of the Moroccan Anti-Atlas Mountains, the Alnif area exposes a buried Ordovician glacial tunnel valley (5 km wide, 180 m deep) cut into preglacial marine sediments. The preglacial sedimentary sequence, deposited in a marine environment, is characterized by a typical "layer-cake" configuration of permeable (sand) and impermeable (clays and early-cemented sandstones) layers. At the base of the tunnel valley, a discontinuous and fan-shaped glacial conglomeratic unit 10 to 15 m thick occurs, erosively deposited over preglacial marine sediments. The conglomeratic unit is composed of preglacial intraclasts embedded within a sandy matrix. Both …

SubglacialgeographyTunnel valleyTunnel valleygeography.geographical_feature_categorySediment remobilizationStratigraphyOrdovician[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/GlaciologyGeochemistryGeology[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPorewater pressureConglomerate[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyClastic rockSedimentary rock[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/GlaciologyGlacial periodHydrofracturingIce sheetMeltwaterIntraclastsGeomorphologyGeologySedimentary Geology
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Hybrid Energy Storage for Underground Mining EV

2021

One of the main concerns when it comes to contributions to the carbon footprint is the consumption of fuel by vehicles, more specifically that of mining vehicles. One solution to this problem is replacing the combustion engine vehicles with electric vehicles. This also poses the problem of low power density. This paper proposes a solution of using supercapacitors and hybrid capacitors with the aim of investigating how they can affect the performance of electric vehicles. For this purpose, a background of fuel consumption and alternative solutions to the problem are discussed, a prototype was designed and built. It was found that when supercapacitors and hybrid capacitors were used in combin…

SupercapacitorBattery (electricity)Computer sciencebusiness.industryFossil fuelUnderground mining (hard rock)CombustionAutomotive engineeringlaw.inventionCapacitorHardware_GENERALlawFuel efficiencyCarbon footprintbusiness2021 IEEE International IOT, Electronics and Mechatronics Conference (IEMTRONICS)
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Petro-mineralogical controls on coda attenuation in volcanic rock samples

2021

SUMMARY Seismic attenuation measurements, especially those obtained from coda decay analysis, are becoming a key data source for the characterization of the heterogeneous Earth due to their sensitivity to small-scale heterogeneities. However, the relation between the scattering attenuation measured from coda waves and physical rock properties is still unclear. The goal of this study is to identify the main petrophysical and mineralogical factors controlling coda attenuation in volcanic rocks at the laboratory scale, as a necessary step before modelling seismic waves in real volcanic media. Coda wave attenuation was estimated from ultrasonic S-wave waveforms. To quantify the heterogeneity of…

Supplementary datageographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLibrary science010502 geochemistry & geophysics01 natural sciencesData availabilityCodaVolcanic rockGeophysicsGeochemistry and PetrologyGeology0105 earth and related environmental sciencesGeophysical Journal International
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Origin and Evolution of High-Grade Gneiss Terrains

1990

In the previous chapters we have given an impression of the way in which the analysis of high-grade rocks can be approached in the field. Here we conclude with some current larger-scale ideas on the origin and evolution of such rock assemblages.

Supracrustal rockContinental crustGeochemistryTerrainPetrologyGeologyMantle plumeGneiss
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Preliminary results of a geomorphological and DInSAR characterization of a recently identified Deep-Seated Gravitational Slope Deformation in Sicily …

2019

The study is part of a larger project that involves the analysis of recently identified Deep-Seated Gravitational Slope Deformation (DSGSD) in Sicily which have been sub-divided according to the geological framework in light of the new geological data about the regional setting. Here are presented the first results of a multidisciplinary study of a DSGSD recently identify in Mount San Calogero area (Northern Sicily). The study was performed by means of different approaches including conventional methods (field surveys) and the Differential Interferometry Synthetic Aperture Radar (DInSAR) technique. The geological and geomorphological analyses were carried out to investigate slopes dynamic, …

Synthetic aperture radarMonitoringLineamentGeologyLandslideDeformation (meteorology)Displacement (vector)GravitationTectonicsLandslideDeep-seated gravitational slope deformationDInSARRock mass classificationSicilySeismologyGeologyRendiconti Online della Società Geologica Italiana
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Space-borne frequency comb metrology

2016

Precision time references in space are of major importance to satellite-based fundamental science, global satellite navigation, earth observation, and satellite formation flying. Here we report on the operation of a compact, rugged, and automated optical frequency comb setup on a sounding rocket in space under microgravity. The experiment compared two clocks, one based on the optical D2 transition in Rb, and another on hyperfine splitting in Cs. This represents the first frequency comb based optical clock operation in space, which is an important milestone for future satellite-based precision metrology. Based on the approach demonstrated here, future space-based precision metrology can be i…

Synthetic aperture radarPhysicsEarth observationSounding rocketOrders of magnitude (temperature)business.industryPhysics::Optics02 engineering and technology021001 nanoscience & nanotechnology01 natural sciencesAtomic and Molecular Physics and OpticsElectronic Optical and Magnetic MaterialsMetrology010309 opticsFrequency combOpticsPhysics::Space Physics0103 physical sciencesSatelliteSatellite navigation0210 nano-technologybusinessOptica
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Assessment of soil particle erodibility and sediment trapping using check dams in small semi-arid catchments

2017

Check dams can be used as a source of information for studies on sediment characteristics and soil particle erodibility. In this study, sediment yield and grain size distribution (GSD) were measured in twenty small catchments draining into a rock check dam in NW Iran for different runoffs during 2010–2011. Significant correlations were found between sediment yield and slope steepness, vegetation cover and soil erodibility factor (K) of the catchments. The erodibility of soil particles was determined using the comparison of GSD between sediment and original soil. Clay was the most erodible soil particle which showed 2.05 times more percentage in sediment than the original soil. The erodibili…

Sòls Erosió010504 meteorology & atmospheric sciencesGrain size distributioncomplex mixtures01 natural sciencesCement rock check damVegetation coverSediment trapping0105 earth and related environmental sciencesEarth-Surface ProcessesHydrologySediment yieldRemaining capacitySediment yieldSedimentRainfall erosivity04 agricultural and veterinary sciencesBodemfysica en LandbeheerPE&RCAridSoil Physics and Land ManagementParticle-size distribution040103 agronomy & agriculture0401 agriculture forestry and fisheriesParticleGeologyCheck damCATENA
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Towards a dendrochronologically refined date of the Laacher See eruption around 13,000 years ago

2020

Highlights • Previous age estimates of the Laacher See Eruptions (LSE) around 12,900 years are still diverging and imprecise. • The combination of dendrochronology, wood anatomy, and 14C measurements holds the potential to establish a precise LSE date. • An absolute calendric date of the LSE would improve the synchronization of European Late Glacial to Holocene archives. Abstract The precise date of the Laacher See eruption (LSE), central Europe’s largest Late Pleistocene volcanic event that occurred around 13,000 years ago, is still unknown. Here, we outline the potential of combined high-resolution dendrochronological, wood anatomical and radiocarbon (14C) measurements, to refine the age …

TEPHRA010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPleistoceneVARVE CHRONOLOGYPyroclastic rock01 natural scienceslaw.inventionVOLCANIC-ERUPTIONPaleontologylawINTCAL13Glacial periodRadiocarbon datingEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesCALIBRATIONGlobal and Planetary Changegeographygeography.geographical_feature_categorySubfossilGeologyRECORDABRUPT CLIMATE-CHANGEPALAEOLAKEVolcano13. Climate actionMEERFELDER MAARBiologieSEDIMENTSGeologyQuaternary Science Reviews
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On thrusting, regional unconformities and exhumation of high-grade greenstones in Neoarchean orogens. The case of the Waroonga Shear Zone, Yilgarn Cr…

2017

Abstract During the Neoarchean, the dominant tectonic style progressively changed from an episodic-overturn/stagnant-lid regime to modern-style plate tectonics. The Neoarchean strengthening of continental lithosphere changed the style of deformation of orogenic belts. The case study presented here provides insights into how such transition in tectonic style occurred, a matter that is generally controversial. We present structural and metamorphic data from the c. 2660 Ma Waroonga Shear Zone (WSZ) in the Neoarchean Yilgarn orogen (Western Australia). The WSZ contains a syntectonic pluton and older, high-grade greenstones. The tectonic fabric in the pluton developed during melt-present thrusti…

THERMOCALCP–T path010504 meteorology & atmospheric sciencesMetamorphic rockArcheanGeochemistryExhumationYilgarn Craton010502 geochemistry & geophysics01 natural sciencesSynmagmatic shearingTranspressionPlate tectonicsGeophysicsLithosphereHigh-grade greenstoneShear zoneGeomorphologyGeophysicGeology0105 earth and related environmental sciencesTerraneEarth-Surface Processes
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