Métamorphisme | EPFL Graph Search

vignette|upright=1.6|Évolutions métamorphiques les plus souvent enregistrées par les roches du métamorphisme régional en domaine continental, dans le diagramme pression-température (P-T) dans le métamorphisme. Domaines de stabilité de (chlorite, plagioclase, biotite, grenat, andalousite, disthène et sillimanite). Le métamorphisme désigne l'ensemble des transformations subies à l'état solide par une roche (sédimentaire, magmatique ou métamorphique) sous l'effet de modifications des conditions de température, de pression, de la nature des fluides minéralisés ou de la composition chimique de la roche. Ces transformations, qui peuvent être minéralogiques, texturales, chimiques ou encore structurales, provoquent une réorganisation des éléments dans la roche et une recristallisation des minéraux. La roche ainsi transformée est dite métamorphique. L'une des caractérisations les plus directes du métamorphisme est la transformation minéralogique de la roche (avec en cas de métasomatisme, chan

Thermal diffusivity of seasonal snow determined from temperature profiles

Chad Higgins, Wolf Hendrik Huwald, Holly Jayne Oldroyd, Marc Parlange

Thermal diffusivity of snow is an important thermodynamic property associated with key hydrological phenomena such as snow melt and heat and water vapor exchange with the atmosphere. Direct determination of snow thermal diffusivity requires coupled point measurements of thermal conductivity and density, which continually change due to snow metamorphism. Traditional methods for determining these two quantities are generally limited by temporal resolution. In this study we present a method to determine the thermal diffusivity of snow with high temporal resolution using snow temperature profile measurements. High resolution (between 2.5 and 10 cm at 1 min) temperature measurements from the seasonal snow pack at the Plaine-Morte glacier in Switzerland are used as initial conditions and Neumann (heat flux) boundary conditions to numerically solve the one-dimensional heat equation and iteratively optimize for thermal diffusivity. The implementation of Neumann boundary conditions and a ttest, ensuring statistical significance between solutions of varied thermal diffusivity, are important to help constrain thermal diffusivity such that spurious high and low values as seen with Dirichlet (temperature) boundary conditions are reduced. The results show that time resolved thermal diffusivity can be determined from temperature measurements of seasonal snow and support density-based empirical parameterizations for thermal conductivity.

Elsevier2013

Oxygen diffusion in garnet: Experimental calibration and implications for timescales of metamorphic processes and retention of primary O isotopic signatures

Stéphane Laurent Escrig, Anders Meibom

Knowledge of oxygen diffusion in garnet is crucial for a correct interpretation of oxygen isotope signatures in natural samples. A series of experiments was undertaken to determine the diffusivity of oxygen in garnet, which remains poorly constrained. The first suite included high-pressure (HP), nominally dry experiments performed in piston-cylinder apparatus at: (1) T = 1050-1600 degrees C and P = 1.5 GPa and (2) T = 1500 degrees C and P = 2.5 GPa using yttrium aluminum garnet (YAG; Y3Al5O12) cubes. Second, HP H2O-saturated experiments were conducted at T = 900 degrees C and P = 1.0-1.5 GPa, wherein YAG crystals were packed into a YAG + Corundum powder, along with O-18-enriched H2O. Third, 1 atm experiments with YAG cubes were performed in a gas-mixing furnace at T = 1500-1600 degrees C under Ar flux. Finally, an experiment at T = 900 degrees C and P = 1.0 GPa was done using a pyrope cube embedded into pyrope powder and O-18-enriched H2O. Experiments using grossular were not successful. Profiles of O-18/(O-18+O-16) in the experimental charges were analyzed with three different secondary ion mass spectrometers (SIMS): sensitive high-resolution ion microprobe (SHRIMP II and SI), CAMECA IMS-1280, and NanoSIMS. Considering only the measured length of O-18 diffusion profiles, similar results were obtained for YAG and pyrope annealed at 900 degrees C, suggesting limited effects of chemical composition on oxygen diffusivity. However, in both garnet types, several profiles deviate from the error function geometry, suggesting that the behavior of O in garnet cannot be fully described as simple concentration-independent diffusion, certainly in YAG and likely in natural pyrope as well. The experimental results are better described by invoking O diffusion via two distinct pathways with an inter-site reaction allowing O to move between these pathways. Modeling this process yields two diffusion coefficients (D values) for O, one of which is approximately two orders of magnitude higher than the other. Taken together, Arrhenius relationships are: logDm(2)s(-1) = -7.2(+/- 1.3)+(-321(+/- 32)kJ mol(-1))/2.303RT) for the slow pathway, and logDm(2)s(-1) = -5.4(+/- 0.7)+(-312(+/- 20)kJ mol(-1)/2.303RT) for the fast pathway. We interpret the two pathways as representing diffusion following vacancy and interstitial mechanisms, respectively. Regardless, our new data suggest that the slow mechanism is prevalent in garnet with natural compositions, and thus is likely to control the retentivity of oxygen isotopic signatures in natural samples. The diffusivity of oxygen is similar to Fe-Mn diffusivity in garnet at 1000-1100 degrees C and Ca diffusivity at 850 degrees C. However, the activation energy for 0 diffusion is larger, leading to lower diffusivities at P-T conditions characterizing crustal metamorphism. Therefore, original O isotopic signatures can be retained in garnets showing major element zoning partially re-equilibrated by diffusion, with the uncertainty caveat of extrapolating the experimental data to lower temperature conditions.

MINERALOGICAL SOC AMER2022

Oxygen diffusion in garnet: Experimental calibration and implications for timescales of metamorphic processes and retention of primary O isotopic signatures

Stéphane Laurent Escrig, Anders Meibom

MINERALOGICAL SOC AMER2022