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215 results for “Slab”
Killodiernan Trial Slab (SMR No. TN009-040005-)
Sandstone slab lying against inner face of southern wall at the east end of Killodiernan Romanesque Church ruins (TN009-040001-) in North Tipperary. The stone has a poorly executed pocked carving consisting of three poorly drawn circles the centre of which are bisected by a poorly excecuted incised horizontal line. The purpose of this stone is unknown and may have been a trial piece to teach how to carve onto a stone surface. The pock marks of the tool used to carve the circles and the line are clearly visible on the 3D model. The name Killodiernan is translated as the church of the O'Tiernans and the Cill placename may suggest an early medieval date for the church site. For more information on the stone slab, visit: https://maps.archaeology.ie/HistoricEnvironment/?SMRS=TN009-040005- Source: Objaverse 1.0 / Sketchfab
Portal dolmen slab with knobs
Portal dolmen slab with knobs The dolmen is located on Mezetsu range (Priyut group of monuments), Sochi region, Caucasus, Russia, Middle Bronze Age (4000-2000 BC), Dolmen Culture of Caucasus. Portal stone slab with four protruding knobs on the upper part. Only the ruins of this dolmen have survived. Фасадная плита дольмена с четырьмя асимметрично расположенными округлыми выпуклостями в верхней ее части. Развал плиточного дольмена, дольменная культура Кавказа, 4-2 тыс. до н.э., средняя бронза. Северо-западный Кавказ, бассейн реки Малый Наужи, группа Приют (урочище Кубыши). Source: Objaverse 1.0 / Sketchfab
Medieval Ringed Cross-Slab (TN009-003003-)
Medieval incised ringed cross-slab (TN009-003003-) with naively carved crucified Christ in centre of cross all of which is framed within an incised border located inside the medieval parish church ruins (TN009-003001-) in Kilbarron graveyard (TN009-003002-), North Tipperary. For more detailed description of the monument, visit: https://maps.archaeology.ie/HistoricEnvironment/?SMRS=TN009-003003- Source: Objaverse 1.0 / Sketchfab
Gallen Cross-Slab (OF014-029152-)
Possible 8th-century cross-slab with a four-lined cross-of-arcs, also forming a cross pattée design, with small central hollow contained within a triple circle recently discovered from Gallen graveyard (OF014-029002-), Co. Offaly. The cross-of-arcs design may be based on the cross surrounded by a wreath, or on the XP monogram contained within a circle. The largest collection of this type of cross-slab comes from Gallen. Gallen abbey (OF014-029001-) stands in the centre of this graveyard that was built near the site of an Early Christian monastery (OF014-029008-) founded by St. Canoc in 492 AD. A group of early Christian cross-slabs (OF014-029003-) dating from the 8th/11th-centuries were uncovered along with the site of an early medieval church (OF014-029008-) during excavations in 1934-5 in a field to the north of the graveyard. Cross-slab has been moved to the National Museum of Ireland for safe storage. For more information, visit: https://maps.archaeology.ie/HistoricEnvironment/?SMRS=OF014-029152- Source: Objaverse 1.0 / Sketchfab
Relif slab. Pentelic Marble.
Found at Epidauros. Probably from an altar of the twelve Olympian God. On the left narrow side is a description of Niki with open winge, which spread on to the front of the slab, while the right side has a description of an Archaistie Female figure holding an oinochoe. 350-325 B.C. or - according to a recent view - work of the 1st st B.C., influenced by 4th c. B.C. originale. Source: Objaverse 1.0 / Sketchfab
Moybologue - Possible Cross Slab
This stone is situated inside the gate of the graveyard to the left. It does not appear to be recorded on the SMR with the other stones at the site. A crosinscribed circle can be seen on it's face. Source: Objaverse 1.0 / Sketchfab
Gellyburn Cross-Slab
Almost complete sandstone Pictish cross-slab from Gellyburn, Murthly, Perthshire. Eighth-ninth century AD. From the collection of Perth Museum & Art Gallery, Perth & Kinross Council. accession number: PERGM 6/1949 780x260x95mm Source: Objaverse 1.0 / Sketchfab
Lorrha Ringed Cross-Slab (TN004-010032-)
Rectangular-shaped early Christian sandstone ringed cross-slab re-used as the base of a 15th century wall cupboard located immediately east of the southern doorway to the chapter house at the eastern end of the southern wall of the Augustinian priory (TN004-010006-) in Lorrha, Co. Tipperary. The upper surface of the sandstone slab is decorated with a ringed-cross with hollowed angles carved in false relief with panels of ribbon-interlace on either side of the cross shaft all opf which is contained within an incised framed outline running around the edge of the slab. Lorrha monastery was founded by St. Ruadhán who died in 584 and was referred to as the 'lamp of Lothra', his feastday was held on the 15th of April when the 'cuckoo began to call'. For more information on the cross-slab, visit: https://maps.archaeology.ie/HistoricEnvironment/?SMRS=TN004-010032- Source: Objaverse 1.0 / Sketchfab
Loughrea Cross Slab - 2
This slab is located at the rear of loughrea library which is also the site of St. Brendans Church. Source: Objaverse 1.0 / Sketchfab
Data for: Influence of Anomalous Ocean Heat Transport on the Extratropical Atmospheric Circulation in a High-Resolution Slab-Ocean Coupled Model
<p>This dataset, provided in NetCDF format, supports the research presented in the paper titled "Influence of Anomalous Ocean Heat Transport on the Extratropical Atmospheric Circulation in a High-Resolution Slab-Ocean Coupled Model." Please contact Dr. Sun (ltsun@rams.colostate.edu) if you have any questions.</p>
Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet
<p>Data used to generate figures published in Strak et al. (2024) in the journal Communications Earth & Environment (LINK).</p>
Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events: scripts and data
<p>The files provided here supplement the following article which has been conditionally accepted to Gondwana Research:</p> <p>'Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events'</p> <p>Both the scripts used to generate the work presented in the study, as well as the data/results, have been included in the attached zipped folders.</p>
Dataset for the paper "Direct prediction of saturated neoclassical tearing modes in slab using an equilibrium approach"
<p>Data and scripts related to the publication "Direct prediction of saturated neoclassical tearing modes in slab using an equilibrium approach".</p>
Porphyry copper formation driven by water-fluxed crustal anatexis during flat-slab subduction
<p><span>Supplemtary Data used in the study entitled 'Lamont et al. (2024) Porphyry copper formation driven by water-fluxed crustal anatexis during flat-slab subduction, Nature Geoscience'.</span></p> <p><span>A compilation of geochronology (U–Pb and Ar-Ar and K-Ar) for intrusive and extrusive igneous rocks, mineralization and porphyry copper deposits, and timing of shortening and extension is provided in Supplementary Table S1. Whole rock geochemical data from igneous rocks in Arizona is provided in Supplementary Table 2. A compilation of Nd, Pb and Hf in zircon isotopes, and two-stage model ages from the SW USA and NW Mexico is provided in Supplementary Table S3. Electron-probe microanalysis data for samples TLAZ22-08 and TLAZ22-167 are in Supplementary Table S4. Thermobarometry Results are provided in Supplementary Table S5. In-situ Rb-Sr Geochronology Results are provided in Table S6, whereas U–Th–Pb Monazite Geochronology Results are provided in Supplementary Table S7. <span> </span></span></p>
Topography Response to Horizontal Slab Tearing and Oblique Continental Collision: 3D Thermomechanical Numerical Modelling
<p>This repository submission provides the 3D thermo-mechanical numerical modelling code I3ELVIS developed by the workgroup of Prof. Taras Gerya (ETH Zürich). The code is based on finite-difference and marker-in-cell methods (Gerya & Yuen, 2003, 2007; Gerya, 2019). The code solves the momentum, continuity, and energy equations on the fixed Eulerian grid and transports the physical properties by Lagrangian markers using the velocity field. The code also accounts for the major phase transitions in the Earth’s mantle and internal heat sources arising from adiabatic, radiogenic, and frictional heating. Partial melting and melt extraction processes are neglected for the sake of simplicity. A more detailed description of the code, including the governing equations and the adopted rheological model can be found in various published literature (Andrić-Tomašević et al., 2023; Boonma et al., 2023; Maiti et al., 2024). Interested users are recommended to contact Prof. Taras Gerya (taras.gerya@erdw.ethz.ch). </p> <p>The repository also provides input and output files to run and reproduce model results and manuscript figures of Maiti et al., 2024 (JGR Solid Earth). Paraview States for processing .vtr result files and visualizing the model output data. Matlab script to visualise the topography from .grd files. </p>
The 2021-2022 Fukushima-Oki Earthquakes in Northeastern Japan: Dehydration Triggered Fault Reactivation Boosted by Slab Segmentation
<p>codes.rar: codes of double-difference seismic tomography</p> <p>catalog.dat: earthquake phase catalog used in the DD tomography</p> <p>station.dat: station coordinates of the seismic network </p> <p>MOD: grids in the initial Vp and Vp/Vs models</p> <p>Vp_model.dat: inverted 3-D Vp model</p> <p>Vs_model.dat: inverted 3-D Vs model</p> <p>VpVs_model.dat: inverted 3-D Vp/Vs model</p> <p>earthquake.reloc: relocations of the earthquakes</p>
Automated Earthquake Catalogues for CHARGE & CHARSME/CSN networks in South America (Pampean Flat Slab)
<p>This repository includes:</p> <p>1. Gzipped automated catalogues of earthquake locations with P and S arrival times for:</p> <ul> <li>The CHARGE network - charge.data.gz</li> <li>The CHARSME and CSN networks - charsme_csn.data.gz</li> </ul> <p>2. A README explaining the information in each column </p>
Ptatin2D : dataset for run simulations presented in the article Slab pull driven South China Sea opening implies a Mesozoic Proto South China Sea
<p>Overview of pTatin2D</p> <p>pTatin2D is a software package designed for studying long time-scale processes relevant to geodynamics. The original motivation for this development was to provide the community with an open-source toolkit capable of studying high-resolution, two-dimensional models of lithospheric deformation.</p> <p>Functionality</p> <ul> <li>mixed finite elements (Q2-P1_disc) for the Stokes problem</li> <li>material points for tracking Lagrangian state and history variables</li> <li>energy equation solved with Q1 elements + SUPG</li> <li>ALE formulations (with a variety of remeshing solutions)</li> <li>extensible rheology components (currently supports: iso-viscous, Frank-Kamenetskii, Arrhenius, power-law, von Mises, Drucker Prager)</li> <li>full support for spatio-temporal Dirichlet and non-zero Neumann boundary conditions</li> <li>coupling with landscape evolution models</li> <li>full support for Newton and Picard non-linear solvers</li> <li>massively parallel implementation</li> </ul> <p>pTatin2D leverages functionality from <a href="http://www.mcs.anl.gov/petsc">PETSc</a></p> <p>Requirements</p> <ul> <li>PETSc (only support for version 3.2)</li> </ul>
Simulation of the Moving Boundary during Freezing of a One-Dimensional Food Slab
<p>To calculate the moving boundary (MB) of a finite 1D moist food slab, which is cooled by convection at the exposed surface, a finite difference model was employed, invoking the Stefan condition. The primary objective of this project was to generate synthetic data comprising MB position-time pairs. The MB time profiles were generated using a nearly orthogonal array, which accounts for the effects of the Biot number, dimensionless cooling-medium temperature, dimensionless latent heat, and thermal conductivity parameter. The last two parameters play a crucial role in controlling the temperature dependence of the effective heat capacity and thermal conductivity of the food material. The generated data will be utilized to develop statistical models of the MB, effectively accounting for the influence of temperature-dependent thermal properties</p>
A weak subducting slab at intermediate depths below northeast Japan
<p>Knowledge of the state of stress in subducting slabs is essential for understanding their mechanical behavior and the physical processes that generate earthquakes. Here we develop a novel framework that uses a high-resolution focal mechanism catalog to determine, for the first time, the full deviatoric stress tensor within the subducting slab at intermediate depths. We show that by combining the static stress calculated from coseismic slip distributions with the stress orientations before and after the mainshock, that deviatoric stress within the slab at intermediate depths must be very low ( ∼ 1 MPa). These results preclude earthquake source mechanisms that require large background driving stresses, favoring a mechanically weak subducting slab, thus providing quantitative constraints on the physical processes that generate intermediate-depth earthquakes.</p>
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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.