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84 results for “Metamorphism”
Output files of the Wd_WD model from Baïsset et al. paper entitled « Weakening induced by phase nucleation in metamorphic rocks: insights from numerical models »
<p>Here you can find the Output files of the Wd_WD Model.</p> <p>These files can be read using the files "ReadHDF5_Baisset2024.m" provided with the code here: </p> <p>https://doi.org/10.5281/zenodo.11473988</p>
Output files of the reference model from Baïsset et al. paper entitled « Weakening induced by phase nucleation in metamorphic rocks: insights from numerical models »
<p>Here you can find the Output files of the Reference Model.</p> <p>These files can be read using the files "ReadHDF5_Baisset2024.m" provided with the code here: </p> <p>https://doi.org/10.5281/zenodo.11473988</p> <p> </p>
Development and survival of tadpoles and metamorphs of Rana temporaria in six boreal lakes in southern Finland
<p>We assessed the effect of water colour on the development of larval amphibian. Tadpoles of Rana temporaria were raised in experimental cages in 6 boreal lakes representing a gradient of water colour.</p> <p>The dataset includes the recording of the environmental variables in the lake during the experiment, morphometric variables for tadpoles and metamorphs, as well as tabulated data for survival analysis during the tadpole stage and to metamorphosis. The experiment took place from May to July 2023 in Evo Natural 2000 site in Finland.</p>
Dataset for Formation of Metamorphic Soles underlying Ophiolites during Subduction Initiation: A Systematic Numerical Study
<p>The numerical model results in the paper 'Formation of Metamorphic Soles underlying Ophiolites during Subduction Initiation: A Systematic Numerical Study'.</p>
Structural analysis and peak-metamorphic temperatures across the Kodiak accretionary complex
<p>Here, we report structural analysis (Table S1) and RSCM temperatures (Table S2) of each examined locality across the Kodiak accretionary complex. The reader is referred to the Methods section for a detailed description of the analytical protocols.</p> <p><strong>Contents of this file</strong></p> <p>Table S1 - The dataset of sample locations, observed micro- and mesostructures and stress regime.</p> <p>Table S2 - RSCM temperatures across the Kodiak accretionary complex with previously published results. VR - Vitrinite reflectance; IC - Illite crystallinity; FI - Fluid inclusion studies; MP – Mineral paragenesis.</p>
Thermal state, slab metamorphism and interface seismicity in the Cascadia subduction zone based on 3-D modeling
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Data from: Hindered and constrained: limited potential for thermal adaptation in post-metamorphic and adult Rana temporaria along elevational gradients
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Data from: Correlated evolution of phenotypic plasticity in metamorphic timing
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Data from: Post-metamorphic carry-over effects of larval digestive plasticity
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Data from: Brain plasticity over the metamorphic boundary: carry-over effect of larval environment on froglet brain development
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Thermal regime and petrologic metamorphism in Alaska: Implications for subduction interface and wedge earthquakes
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Slab metamorphism and interface earthquakes in Peru: implications for along-strike fluid content and seismotectonic variation
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Data from: Matriline effects on metamorphic traits in a natural system in the European common frog (Rana temporaria)
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Data from: Artificial light at night decreases metamorphic duration and juvenile growth in a widespread amphibian
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Data from: Diet-induced plasticity modifies relationships between larval growth rate and post-metamorphic behavior and physiology
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Larval and metamorph traits of cane toads
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Two metamorphic gold mineralization events confirmed by Lu-Hf isotope dating of garnet in the Late Archean Storø Au deposit, Nuuk region of SW Greenland
<p><strong>Supplementary material</strong></p> <p><strong>Table A1.</strong> LA-ICP-MS data for a profile through a representative garnet from sample KSZ 21.</p> <p> </p> <p><strong>Table A2.</strong> Lu-Hf isotope data for garnet separates. The samples are described in Szilas et al. (2014).</p> <p> </p> <p><strong>Table A3.</strong> Lu-Hf isotope data for bulk-rock samples. The samples are described in Szilas et al. (2016).</p>
The potential for low-grade metamorphism to facilitate fault instability in a geothermal reservoir
<p>Swarms of earthquakes during shale gas exploitation in the Changning area of the Sichuan Basin indicate that hydraulic fracturing induces seismicity both within the target reservoir formation but also to depths of several kilometers below the horizontal well. These remote earthquakes are possibly triggered by total stress perturbations resulting from the hydraulic fracturing. We use a dislocation-based analytical model to simulate multistage hydraulic fracturing of three horizontal wells at a single well pad to explore the spatiotemporal evolution of the total stress perturbations. Results show that the number and distribution of fracturing stages affect both the distribution and magnitude of stress changes and that the stress change diminishes with distance. The undrained injection-induced stress change is less than 10<sup>-3</sup> <i>MPa</i> at distances ≥1 <i>km</i> for single-stage fracturing but reach 10<sup>-1</sup> <i>MPa</i> for multistage fracturing of 30 stages in all three wells. Undrained stress changes scale linearly with the magnitude of fluid leak-off into the formation – halving the effective fracture width halves the induced stress magnitudes and with an identical distribution – limiting the potential for fault reactivation. Scaling analysis for pressure diffusion distal from the reservoir indicates that the short-term (days to weeks) impact is indeed essentially undrained. Estimates for long-term reservoir depletion (months to years) identify a similar induced stress signal of opposite sign but with similar Coulomb potential for reactivation in the long term. Such magnitudes of Coulomb stress changes suggest the possibility of fault reactivation on deep critically-stressed faults at kilometer separation from the injection both in the short term due to stimulation and in the long term as a result of reservoir depletion.</p>
Kinematic, Metamorphic and Age Constraints on the Miyar Thrust Zone: Implications for the Eohimalayan History of the High Himalayan Crystalline of NW India
<p>Table 1: Instrumental setup and operating conditions during the LA-ICP-MS analyses</p> <p>Table 2: U/Th-Pb Analytical Data</p> <p> </p>
Supporting dataset of the reaction zones and marbles in the Mogok metamorphic belt
<p>The datasets include six tables. These tables include the information on the sample description, compositions of whole rocks and minerals, U-Th-Pb isotope data of baddeleyite and zircon, and mass-transfer calculation results for polycrystalline mineral reaction zones (PMRZs) in dolomite marbles from the Mogok metamorphic belt, Myanmar. The whole-rock compositions were determined by XRF and ICP-MS. The major elements of minerals were analyzed by EPMA, whereas the trace elements of minerals were analyzed by LA-ICP-MS. The U-Th-Pb isotope data were measured by SIMS.</p>
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Allen Brain Atlas
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International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.