Search results for "petrol"

showing 10 items of 1738 documents

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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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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Textural-chemical changes and deformation conditions registered by phyllosilicates in a fault zone (Pic de Port Vieux thrust, Pyrenees)

2017

International audience; Synkinematic phyllosilicates in fault zones can be used to deduce the deformation mechanisms and the conditions of fault activity, as their chemical composition, crystal structure and texture can record the different stages of deformation and fluid-rock interactions. The Pic de Port Vieux, a second-order thrust related to the major Gavarnie thrust in the southern central part of the Pyrenees Axial Zone, juxtaposes Triassic pelites of the hanging wall and Cretaceous limestones of the footwall. In order to investigate the mineralogical and geochemical changes and constrain the deformation conditions of thrusting, characterization of phyllosilicates was performed along …

010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]GeochemistryFault (geology)engineering.material010502 geochemistry & geophysics01 natural sciences[ SDE ] Environmental Scienceschemistry.chemical_compoundGeochemistry and PetrologyPeliteThrust faultQuartzChlorite0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryK-white micaThrust fault[ SDV ] Life Sciences [q-bio]MuscovitePyreneesGeologyHematitePhyllosilicatesFluid-rock interactionsDiagenesischemistry[SDU]Sciences of the Universe [physics]visual_art[SDE]Environmental Sciencesvisual_art.visual_art_mediumengineeringChloriteGeology[ SDU ] Sciences of the Universe [physics]
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Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?

2021

Abstract The expansion of land plants is considered to have played a key role in triggering the Late Paleozoic Ice Age (LPIA), but evidence linking climatic events to terrestrial floral changes is limited. Here, we generated bulk carbonate δ13C, conodont δ18O and 87Sr/86Sr profiles from the lowermost Carboniferous of South China and Vietnam in order to investigate their relationship to contemporaneous land plant evolution. Climatic cooling in the mid-Tournaisian coincided with large perturbations to the global carbon cycle and continental weathering regimes as well as with a major diversification episode among seed plants. These relationships are consistent with terrestrial floral changes t…

010504 meteorology & atmospheric sciencesbiologyPaleozoicEarth scienceClimate changeWeathering15. Life on land010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCarbon cycleGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyCarboniferousEarth and Planetary Sciences (miscellaneous)Ice ageConodontGlobal coolingGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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A sugar biomarker proxy for assessing terrestrial versus aquatic sedimentary input

2016

Abstract One of the most important and at the same time most challenging issues in paleolimnological research is the differentiation between terrestrial and aquatic sedimentary organic matter (OM). We therefore investigated the relative abundance of the sugars fucose (fuc), arabinose (ara) and xylose (xyl) from various terrestrial and aquatic plants, as well as from algal samples. Algae were characterized by a higher abundance of fucose than vascular plants. Our results and a compilation of data from the literature suggest that fuc/(ara + xyl) and (fuc + xyl)/ara ratios may serve as complementary proxies in paleolimnological studies for distinguishing between terrestrial and aquatic sedimen…

010504 meteorology & atmospheric sciencesbiologyXylose010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleolimnologyFucosechemistry.chemical_compoundAlgaechemistryGeochemistry and PetrologyAquatic plantBotanySedimentary organic matterSugarRelative species abundance0105 earth and related environmental sciencesOrganic Geochemistry
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Decrespignyite-(Y), a new copper yttrium rare earth carbonate chloride hydrate from Paratoo, South Australia

2002

AbstractDecrespignyite-(Y) is a new copper yttrium rare earth carbonate chloride hydrate from the Paratoo copper mine, near Yunta, Olary district, South Australia. Decrespignyite-(Y) occurs as blue crusts, coatings and fillings in thin fissures on the slatey country rock. Individual pseudohexagonal platelets are typically 10–50 µm in maximum dimension and are often curved. Associated minerals include caysichite-(Y), donnayite-(Y), malachite and kamphaugite-(Y). Electron microprobe and CHN analyses gave: Y2O3 42.2; La2O3 0.1; Pr2O3 0.1; Nd2O3 1.3; Sm2O3 1.0; Gd2O3 4; Tb2O3 0.4; Dy2O3 3.7; Ho2O3 2.6; Er2O3 2.5; CaO 0.5; CuO 10.9; Cl 3.0; CO2 19.8; H2O 10.8, yielding an empirical formula of (Y…

010504 meteorology & atmospheric scienceschemistry.chemical_elementMalachiteElectron microprobeYttrium010502 geochemistry & geophysics01 natural sciencesCopperchemistry.chemical_compoundCrystallographychemistryGeochemistry and Petrologyvisual_artvisual_art.visual_art_mediumPleochroismCarbonateHydratePowder diffraction0105 earth and related environmental sciencesMineralogical Magazine
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Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust

2013

Many unresolved questions in geodynamics revolve around the physical behaviour of the two-phase system of a silicate melt percolating through and interacting with a tectonically deforming host rock. Well-accepted equations exist to describe the physics of such systems and several previous studies have successfully implemented various forms of these equations in numerical models. To date, most such models of magma dynamics have focused on mantle flow problems and therefore employed viscous creep rheologies suitable to describe the deformation properties of mantle rock under high temperatures and pressures. However, the use of such rheologies is not appropriate to model melt extraction above …

010504 meteorology & atmospheric sciencescrust and lithosphere; Pluton emplacement [Fracture and flow; Dynamics of lithosphere and mantle; Mechanics theory and modelling; Rheology]CrustGeophysicsMagma chamberDiapirGeodynamics010502 geochemistry & geophysics01 natural sciencesMantle (geology)TectonicsGeophysicsShear (geology)13. Climate actionGeochemistry and PetrologyLithosphereGeology0105 earth and related environmental sciencesGeophysical Journal International
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Phase equilibrium constraints on pre-eruptive conditions of recent felsic explosive volcanism at Pantelleria Island, Italy.

2010

International audience; We present experimental phase equilibria carried out on a pantelleritic bulk-rock composition with a peralkalinity index [PI = molar (Na2O + K2O)/Al2O3] = 1*4, which is representative of the most energetic pumice fall eruption of the resurgent post-caldera volcanism on Pantelleria island. For the explored conditions (P = 25-150 MPa; T = 680-800°C; H2Omelt up to 6 wt %; fO2 ≤ NNO, where NNO is nickel-nickel oxide buffer) clinopyroxene is the liquidus phase followed by alkali feldspar and then quartz. The crystallization of amphibole is limited to temperatures below 700°C. Aenigmatite crystallizes near the liquidus for P ≥ 100 MPa. When clinopyroxene is the sole liquid…

010504 meteorology & atmospheric sciencespantellerite[SDE.MCG]Environmental Sciences/Global Changeshydrous reduced magmaLiquidusengineering.material010502 geochemistry & geophysicsFeldspar01 natural sciencesPeralkaline rockAenigmatiteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyphase equilibriaPetrologyGeomorphology0105 earth and related environmental sciencesMelt inclusionsFelsicSettore GEO/07 - Petrologia E PetrografiaGeophysics13. Climate actionvisual_artMagmaengineeringvisual_art.visual_art_mediumperalkaline magmatismAlkali feldsparGeologyPantelleria
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Experimental Constraints on the Crystallization of Silica Phases in Silicic Magmas

2021

Abstract Low-pressure silica polymorphs, e.g. quartz (Qtz), tridymite (Trd), and cristobalite (Crs), are common in silicic magmas, but the conditions of their formation are still unclear. The stability fields of these polymorphs have been determined in the SiO2, SiO2–H2O, and haplogranite systems, but these simple systems are not directly applicable to silica polymorph crystallization in natural silicic magmas. The present study compiles an experimental database of new and previously-published data documenting the crystallization of silica phases in natural silicic magmas and simple synthetic systems. Silica polymorphs are identified using Raman spectroscopy and their pressure-temperature d…

010504 meteorology & atmospheric sciencessilica polymorphcrystallizationSilicic[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural scienceslaw.inventionmetastabilityGeophysicsChemical engineeringeruptive dynamicsGeochemistry and Petrologylaw[SDU]Sciences of the Universe [physics][SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCrystallizationGeologysilicic magma0105 earth and related environmental sciences
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Rare earth element and neodymium isotope tracing of sedimentary rock weathering

2020

Chemical weathering plays an important role in sequestering atmospheric CO2, but its potential influence on global climate over geological timescales remains debated. To some extent, this uncertainty arises from the difficulty in separating the respective contribution of sedimentary and crystalline silicate rocks to past weathering rates in the geological record; two types of rocks having presumably different impact on the long-term carbon cycle. In this study, we investigate the use of rare earth element (REE) and neodymium isotopes (εNd) in leached iron oxide fractions of river sediments for tracing the origin of weathered rocks on continents. A new index, called ‘concavity index’ (CI), i…

010504 meteorology & atmospheric sciencessub-01Mid-REE enrichmentGeochemistrySilicate weatheringWeatheringConcavity indexengineering.materialStructural basin010502 geochemistry & geophysicsGeologic record01 natural sciencesIron oxideschemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[CHIM]Chemical Sciences0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySulphide weatheringNeodymium isotopesGeology15. Life on landWorld riversSilicateCratonchemistry13. Climate actionCarbonate weatheringengineeringCarbonateSedimentary rockPyriteGeology
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