Search results for "MINERALOGY"

showing 10 items of 1516 documents

Growth of stylolite teeth patterns depending on normal stress and finite compaction

2007

Abstract Stylolites are spectacular rough dissolution surfaces that are found in many rock types. They are formed during a slow irreversible deformation in sedimentary rocks and therefore participate to the dissipation of tectonic stresses in the Earth's upper crust. Despite many studies, their genesis is still debated, particularly the time scales of their formation and the relationship between this time and their morphology. We developed a new discrete simulation technique to explore the dynamic growth of the stylolite roughness, starting from an initially flat dissolution surface. We demonstrate that the typical steep stylolite teeth geometry can accurately be modelled and reproduce natu…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph][SDE.MCG]Environmental Sciences/Global ChangesCompactionFOS: Physical sciencesMineralogyGeometry[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Surface finish010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsPhysics - GeophysicsStress (mechanics)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)Scaling0105 earth and related environmental sciencesElastic energyDissipation[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpeGeophysics (physics.geo-ph)GeophysicsAmplitudeSpace and Planetary ScienceStyloliteGeologyEarth and Planetary Science Letters
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Modelling of stylolite geometries and stress scaling

2012

International audience; In this contribution we present numerical simulations of stylolite growth to decipher the effects of initial rock heterogeneity and stress on their morphology. We show that stylolite growth in a rock with a uniform grain size produces different patterns than stylolite growth in a rock with a bimodal grain size distribution. Strong pinning of large heterogeneities produce stylolite structures that are dominated by pronounced teeth, whereas a uniform grain size leads to spikes and a roughness that shows variable wavelengths. We compare the simulated stylolites with natural examples and show that the model can reproduce the real structures. In addition we show that stro…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]stress-gauge[SDE.MCG]Environmental Sciences/Global ChangesCompaction[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Surface finishpressure solution010502 geochemistry & geophysics01 natural sciencesPhysics::Geophysics[PHYS.MECA.MEMA]Physics [physics]/Mechanics [physics]/Mechanics of materials [physics.class-ph]Stress (mechanics)Geochemistry and Petrology[SPI.MECA.MEMA]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Mechanics of materials [physics.class-ph]Earth and Planetary Sciences (miscellaneous)compactionGeotechnical engineeringScaling0105 earth and related environmental sciencesstyloliteMechanicsself-affinityGrain sizeGeophysicsSpace and Planetary ScienceStyloliteParticle-size distributionPressure solutionnumerical modelGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyEarth and Planetary Science Letters
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Influence of microporosity distribution on the mechanical behavior of oolithic carbonate rocks.

2015

Abstract The mechanical behavior of oolithic carbonate rocks was investigated for selected rocks with two different microstructural attributes: uniform (UP) and rimmed (RP) distribution of microporosity within ooids. These oolithic carbonate rocks are from the Oolithe Blanche formation, a deep saline aquifer in the Paris Basin, and a possible target for CO2 sequestration and geothermal production. Samples of similar physical properties (porosity, grain diameter, cement content) but different microporosity textures were deformed under triaxial configuration, in water saturated conditions, at 28 MPa of confining pressure, 5 MPa of pore pressure and at a temperature of 55 °C. During the experi…

010504 meteorology & atmospheric sciences[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesTortuosityPore water pressureBrittlenessRock mechanicsMicroporosityParis BasinComputers in Earth SciencesOolithe Blanche formationSafety Risk Reliability and QualityPorosity0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/PetrographyCarbonate rockGeotechnical Engineering and Engineering GeologyOverburden pressurePermeability (earth sciences)Rock mechanics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonate rockGeology
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Trace element behaviour in seawater during Etna's pyroclastic activity in 2001: Concurrent effects of nutrients and formation of alteration minerals

2010

volcanic ash ; trace element leaching ; kinetic experiments ; chlorophyll-alpha; International audience; The eruption of Etna in Sicily on 13 July 2001 marked the most intense activity of the volcano in the last 300 years. The eruption occurred while the oceanographic cruise ANSIC 01 was being conducted to the east of Sicily, presenting a unique opportunity for the investigation of the chemical effects on the marine system during a period of significant (similar to 1 g m(-2)) ash deposition. Comparison of trace element data with measured concentrations from the oceanographic cruise JUVENILE 99, carried out two years before, indicates large enrichments of V. Cr, Mn, Fe, Co, Cu and Pb. We att…

010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesPyroclastic rockMineralogy010502 geochemistry & geophysics01 natural sciencesWater columnGeochemistry and Petrology14. Life underwaterLeaching (agriculture)Kinetic experiment0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryChlorophyll-αTrace elementGeophysicsDeposition (aerosol physics)Volcano13. Climate actionEnvironmental chemistryTrace element leachingSeawaterVolcanic ashGeologyVolcanic ashJournal of Volcanology and Geothermal Research
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Natural gas hydrate investigations by synchrotron radiation X-ray cryo-tomographic microscopy (SRXCTM)

2008

[1] We report the 3D microstructure analyses of natural gas hydrates sampled from Gulf of Mexico. The samples were characterized by synchrotron radiation X-ray cryo-tomographic microscopy (SRXCTM) using the ‘TOMCAT’ beam line at the Swiss Light Source (SLS). The SRXCTM demonstrates its applicability to unlock some microscopic features of the marine hydrates, in particular of crystallite size and grain boundary network. The gas hydrate domains are surrounded by a network of pores of typically a few micrometers, which are largely due to decomposition. Out of the SRXCTM data, the porosity, total volume of the voids, the void surface area and number of the total gas-filled voids have been calcu…

010504 meteorology & atmospheric sciencesbusiness.industryClathrate hydrateSynchrotron radiationMineralogy010502 geochemistry & geophysics01 natural sciencesGeophysicsNatural gasGeneral Earth and Planetary SciencesGrain boundaryCrystallitePorositybusinessHydrateGeologySwiss Light Source0105 earth and related environmental sciencesGeophysical Research Letters
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Characterization of a Newly Developed Aircraft-Based Laser Ablation Aerosol Mass Spectrometer (ALABAMA) and First Field Deployment in Urban Pollution…

2011

We present here the development and first field deployment of a novel Aircraft-based Laser ABlation Aerosol MAss spectrometer (ALABAMA), which is capable of measuring the chemical composition and size of individual ambient aerosol particles in the size range between 150 and 900 nm. The instrument uses a continuous wave 532 nm laser to size and detect the particles, a pulsed 266 nm laser to ablate and ionize the particles, and a bipolar, Z-shaped time-of-flight mass spectrometer to detect positive and negative ions. The ALABAMA fits into a 19"-aircraft rack of 150 cm height and has a total weight of 140 kg, thus currently being one of the smallest and lightest-weight instruments of its type.…

010504 meteorology & atmospheric sciencesinstrument developmentaerosolMineralogy01 natural scienceslaw.inventionOpticslawparticle composition11. SustainabilityEnvironmental ChemistryGeneral Materials ScienceParticle beam0105 earth and related environmental sciencesRange (particle radiation)Laser ablationbusiness.industryChemistry010401 analytical chemistryAtmosphärische SpurenstoffeLaserPollution0104 chemical sciencesAerosol13. Climate actionMass spectrumParticleParticle sizeAerosol Mass spectrometerbusinessAerosol Science and Technology
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Impact of Coseismic Frictional Melting on Particle Size, Shape Distribution and Chemistry of Experimentally-Generated Pseudotachylite

2020

In natural friction melts, or pseudotachylites, clast textures and glass compositions can influence the frictional behavior of faults hosting pseudotachylites, and are, in turn, sensitive to the processes involved in pseudotachylite formation. Quantification of these parameters in situations where the host rock composition and formation conditions are well-constrained, such as analogue experiments, may yield calibrations that can be employed in analysis of natural pseudotachylites. In this paper, we experimentally-generated pseudotachylites in granitoid rocks (tonalite and Westerly granite) at Pconf= 40 MPa and slip rates of ∼0.1 m s−1, comparable to the conditions under which natural pseud…

010504 meteorology & atmospheric sciencessize and shape distributionfrictional meltingMineralogySlip (materials science)engineering.materialchemistry010502 geochemistry & geophysicsFeldspar01 natural sciencesexperimental pseudotachylitePlagioclaselcsh:ScienceQuartzgranite0105 earth and related environmental sciencestonaliteDecrepitationClastic rockvisual_artengineeringvisual_art.visual_art_mediumGeneral Earth and Planetary Scienceslcsh:QComminutionBiotiteFrontiers in Earth Science
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Structural contacts in subduction complexes and their tectonic significance: the Late Palaeozoic coastal accretionary wedge of central Chile

2007

Understanding the contact between the very low-grade metagreywacke of the Eastern Series and high-pressure metamorphosed schist of the Western Series in the Late Palaeozoic accretionary wedge of central Chile is fundamental for the understanding of the evolution of ancient accretionary wedges. We show the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to high-pressure schist of the Western Series at the Pacific coast. Upright chevron folds of sedimentary layering are associated with an axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded abou…

010506 paleontologyAccretionary wedgePaleozoicMineralogy010502 geochemistry & geophysics55101 natural sciencesPaleontologyJungpaläozoikumVAE 50014. Life underwaterChile0105 earth and related environmental sciencesVariszisch-herzynische Orogene {Geologie}SubductionSchistChile {Geologie}Geotektonische Entwicklung der Erdkruste {Geologie}GeologyTectonicsShear (geology)38.36AkkretionskeilFoliation (geology)Sedimentary rockVEX 500VAE 812Geology
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Evidence of aerial volcanic activity during the Valanginian along the northern Tethys margin.

2009

7 pages; International audience; Stratigraphic measurement and sampling on three sections (Vergol, La Charce, and Montclus) through Valanginian deposits from the Vocontian Basin (southeastern France) reveals the occurrence of centimetre thick ochre-coloured layers, which can be correlated from one section to another. At least twelve of these are identified in sediments dated from the Pertransiens to Furcillata ammonite Zones. These horizons appear similar to previously described Oxfordian and Aptian bentonites, also from the Vocontian Basin. Clay-mineralogical and geochemical data are similar in the Valanginian ochre horizons and their enclosing marls except in one of these that shows a cla…

010506 paleontologyAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesBentonite.PaleontologyVolcanismPassive margin[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesAmmoniteHorizon (geology)geographygeography.geographical_feature_categoryPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceousVocontian BasinVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyValanginianlanguageBentoniteGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)

2019

Abstract For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical…

010506 paleontologyArcheologyElemental composition060102 archaeologyOutcropRemainsBuilding stone06 humanities and the artsMineralogyMiddle ages01 natural sciencesArchaeologyRoman periodBuilding stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman periodFortressChemistryPeriod (geology)Carbonate rock0601 history and archaeologyarchaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry0105 earth and related environmental sciencesJournal of Archaeological Science: Reports
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