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215 results for “Slab”
KE035-073024- Loughadoon Cross Slab
Townland: AN CHOILL MHÓR (Bar. Corca Dhuibhne) Scheduled for inclusion in the next revision of the RMP: Yes Description: This large boulder, 1.78m x 1m x .25m thick, has been decorated at either side of its smooth upper surface with a cup-and-3 circles. Beside the E design is a small cup-and-circle with a possible outer circle. The long, linear groove extending NW from the E cup-and-3 circles also appears to be artificial. The stone straddles the low remains of a disused field wall and, if in its original position, suggests an Early Bronze Age or earlier date for the field system. However, it may well have been removed from elsewhere for reuse in the wall. v Source: Objaverse 1.0 / Sketchfab
Paphos, Cyprus. Tomb slab, Latin church in the Chrysopolitissa complex.
<p>Paphos, Cyprus. Tomb slab, Latin church in the Chrysopolitissa complex, made from an antique pillar, split in half; dated 1312. As documented in 1974.</p>
Data for: Slab buckling as a driver for rapid oscillations in plate motion and subduction rate
<p>Data to make the figures in the manuscript: Slab buckling as a driver for rapid oscillations in plate motion and subduction rate by van der Wiel & Pokorny. The readme explains the .txt files.</p>
Cloonacool Cross Slab
Cross slab from Cloonacool Co. Sligo recorded by Ciarian Davis The 'Sligo Community Archaeology Project' is an initiative of Sligo Heritage Forum and is an action of the County Sligo Heritage Plan 2016 – 2020. The project is being undertaken by Sligo County Council in partnership with The Heritage Council and is being delivered by Fadó Archaeology on behalf of the Heritage Office, Sligo County Council. This project received funding from the Heritage Council in 2020. Source: Objaverse 1.0 / Sketchfab
13th-14th century cross-slab fragment
Lower end of tapered cross-slab, chamfered on both sides with a narrow, incised cross with stepped base and three discs on stem. Found in east wall of St James' graveyard - very worn. Recorded by: Orla Power, UCC Digital Humanities Department Funded: Kildare County Council Community Heritage Grant Source: Objaverse 1.0 / Sketchfab
Puulaatta - Slab of Wood
TMK22367:PU1648:039 Vuonna 2006 Tuomiokirkontorin kaivauksilta löytynyt koristeellinen katkennut puulaatta. Alun perin esineeseen on todennäköisesti kuulunut toinen puolikas. Muiden löytöjen perusteella tämä kappale ajoittuu 1400-luvun puoliväliin. A decorated slab of wood that has probably broken into two separate halves. This slab was dug up in 2006 during an excavation at Tuomiokirkontori and is likely from the mid 15th century on the basis of other finds. Source: Objaverse 1.0 / Sketchfab
Gallen Cross Slab OF014-029109-
Possible 8th-century cross-slab with a four-lined cross-of-arcs, also forming a cross pattée design with central hollow, all of which is framed within a triple-lined circle. Gallen was the site of an Early Christian monastery (OF014-029008-) founded by St. Canoc in 492 AD. A large collection 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 at Gallen in 1934-5. This cross-of-arcs type cross-slab is one of nine cross-slabs to come from Gallen monastery. A large selection of cross-slabs were inserted into a display wall on the site of the excavated medieval church. For more information on this cross-slab, visit: https://maps.archaeology.ie/HistoricEnvironment/?SMRS=OF014-029109- Source: Objaverse 1.0 / Sketchfab
TN004-010032 - Cross Slab
Rectangular-shaped early Christian sandstone cross-slab (dims. 0.6m x 0.32m x 0.05m) re-used as stone shelf of aumbry located immediately E of S doorway to chapter house at E end of the S wall of the Augustinian priory (TN004-010006-). The upper surface of the sandstone slab is decorated with a framed ringed-cross with hollowed angles carved in false relief with interlace panels on either side of the cross shaft Source: Objaverse 1.0 / Sketchfab
KE045-009003 - Cross Slab - Kilduff
Description: Kilduff graveyard/Cill Dubh: A rectangular enclosure (KE045-009001-) situated on a steep SSW facing slope at the head of the E-W valley that separates Flemingstown mountain from the central mountain range. Cross-slab (KE045-009003-): This stands near the SE corner of the enclosure and measures 1.13m in height, c. 0.36m in width and c. 0.16m in thickness. The SW face bears an equal-armed cross within a circle, each quadrant thus formed being occupied by a small saltire cross. The lower arm continues beyond the circle and appears to terminate with a scroll or pelta-like motif which is only faintly discernible. The NE face bears a simple equal-armed cross. Two stones set on edge and a large prostrate slab lie W and S of the cross but their function is not known. Source: Objaverse 1.0 / Sketchfab
Moybologue - Cross Slab 2
This cross slab lie inside the main gate of the graveyard to the left. It has a circular enclosed cross on the face with a curved terminal at the top. Source: Objaverse 1.0 / Sketchfab
Loughrea Cross Slab 1
This cross slab is located at the rear of the library in loughrea at the old site of St. Brendans church. Source: Objaverse 1.0 / Sketchfab
Thermal modeling of subduction zones with prescribed and evolving 2D and 3D slab geometries data
<p>Deforming subduction zone finite element model temperature, velocity, surface and flux field data as reported in the work:</p> <p>N. Sime, C. R. Wilson and P. E. van Keken<br> Thermal modeling of subduction zones with prescribed and evolving 2D and 3D slab geometries.</p>
Cryo soft X-ray tomography of 5 microns thick slab extracted from C. elegans midbody region
<p>Samples of C. elegans <span>larvae of strain DM8005 </span>were high pressure frozen using the waffle method. Multiple <span>roughly </span>5 micron thick slabs spanning <span>an L2 larva</span> were extracted using <span>the Serial Lift-Out</span> technique, and placed on rectangular <span>mesh </span>grids. Soft X-ray tomography was performed on individual slabs using the SXT-100 soft x-ray microscope at SiriusXT. The data reveals label free internal structure of fully hydrated C. elegans tissue, annotating the worm volume and adding context to cryo electron tomography data. </p> <p>SXT data was acquired from -50° to +53° in 1° steps and reconstructed using Weighted Back Projection. A 32 nm objective zone plate was used. Data pixel size is 29 nm. </p>
Cryo soft X-ray tomography of 5 microns thick slab extracted from C. elegans anterior region
<p>Samples of C. elegans <span>larvae of strain DM8005 </span>were high pressure frozen using the waffle method. Multiple <span>roughly </span>5 micron thick slabs spanning <span>an L2 larva</span> were extracted using <span>the Serial Lift-Out</span> technique, and placed on rectangular <span>mesh </span>grids. Soft X-ray tomography was performed on individual slabs using the SXT-100 soft x-ray microscope at SiriusXT. The data reveals label free internal structure of fully hydrated C. elegans tissue, annotating the worm volume and adding context to cryo electron tomography data. </p> <p>SXT data was acquired from -50° to +53° in 1° steps and reconstructed using Weighted Back Projection. A 32 nm objective zone plate was used. Data pixel size is 29 nm. </p>
Recorded temperature data of a reinforced concrete, 1.2-m long, beam-slab model and associated meteorological data.
<div><strong>The data contain internal and surface temperature measurements of a 1.2 m-long, reinforced concrete girder-slab element exposed to the environmental conditions of the city of Bucaramanga, Colombia (Coordinates: 7°08'35", 73°07'18"). In addition, meteorological variables of the environment near the element were recorded. The data was measured from July 7, 2023, to November 6, 2023.</strong></div> <div><strong>The data were obtained by:</strong></div> <ul> <li> <div><strong>Internal Temperature (file name: InternalTemperature): 40 thermocouples were embedded in the element (Fig. 1) to collect data every 30 minutes from 6:30 AM on July 10, 2023 to 11:30 PM on November 6, 2023. Temperatures are in degrees Celsius (°C).</strong></div> </li> <li> <div><strong>Surface Temperature (file name: SurfaceTemperatureCameraEast and SurfaceTemperatureCameraWest): A FLIR E6 XT thermal camera was used to record Surface temperature of 10 points on the EAST (Fig. 2) and WEST (Fig. 3) faces of the element from 6:30 AM on June 29, 2023 to 4 PM on October 31, 2023. Twenty daily measurements were recorded every 30 minutes. Temperatures are in degrees Celsius (°C).</strong></div> </li> <li> <div><strong>Surface Temperature (file name: SurfaceTemperatureDroneEast): A DJI MAVIC 2 ENTERPRISE ADVANCED (EU) drone equipped with a thermal imaging camera measured the surface temperature of 10 points on the EAST side of the element (Fig. 4) every 30 minutes, from 6:30 AM on September 9 to 4 PM on October 31. Temperatures are in degrees Celsius (°C).</strong></div> </li> <li><strong>Meteorological variables (file name: WeatherStationData): A DAVIS VANTAGE PRO-2 WLRS weather station recorded data every 30 minutes from 12 AM on July 10, 2023, to 12:30 PM on November 6, 2023. The data included the average, maximum, and minimum ambient temperature (°C); relative humidity (%); speed (m/s) and wind direction (cardinal direction); atmospheric pressure (mb); precipitation (mm) and average and maximum solar radiation (W/m<sup>2</sup>).</strong></li> </ul>
Data for the "Tomographic Imaging of the Pampean Flat Slab: Evidence of Subduction Erosion and Volatile Migration"
<p>This repository includes:</p> <p>1. README - explanation of the information in each column for the datasets<br>2. regional.data.gz - automated catalogue of earthquake locations with P and S arrival times used in the tomography<br>3. surfacewave.data.gz – dispersion curves (ambient noise and "virtual") used in the tomography<br>4. station.list – locations of the seismic stations used in this study<br>5. finmod.ascii.gz - the preferred final model from the tomography (in ASCII format)</p>
Source models for "Across-slab propagation and low stress drops of deep earthquakes in the Kuril subduction zone"
<p>This repository is for the model results for eight deep earthquakes in the Kuril subduction zone modelled using a second-degree moments method in csv format.</p> <p><a href="https://zenodo.org/api/files/ee2b378e-c4a5-4ef0-b07b-e2b2513b3236/Turner_et_al_2022_model_results_subvertical.csv">Turner_et_al_2022_model_results_subvertical.csv</a> - Source models with fixed Amin > 5 km, assuming the sub-vertical fault plane reported in the GCMT catalogue. Event is the GCMT event code. Aspect ratio is the ratio (Amin/Amax). Duration is the rupture duration; Amax is the maximum characteristic fault dimension; Amin is the minimum characteristic fault dimension; Phi is the angle between Amax and the strike; v0 is the centroid velocity; Theta is the angle between the centroid velocity and the strike; and mft is the misfit between the data and the higher-order synthetics calculated for the best-fitting source model obtained from the Monte Carlo inversions.</p> <p> </p> <p><a href="https://zenodo.org/api/files/ee2b378e-c4a5-4ef0-b07b-e2b2513b3236/Turner_et_al_2022_model_results_subvertical.csv">Turner_et_al_2022_model_results_subhorizontal.csv</a> - Source models with fixed Amin > 5 km, assuming the sub-vertical fault plane reported in the GCMT catalogue. Column headers are the same as in <a href="https://zenodo.org/api/files/ee2b378e-c4a5-4ef0-b07b-e2b2513b3236/Turner_et_al_2022_model_results_subvertical.csv">Turner_et_al_2022_model_results_subvertical.csv</a>.</p>
Monte Carlo ray tracing code and simulations for photons scattered by an optically thin slab
<p>This directory contains code and data used to simulate photon path length distributions in an optically thin slab.<br> This material was used to prepare the manuscript "Photon Path Distributions in Optically Thin Slabs" by Quentin Libois and Anthony B. Davis, submitted to Optics Express</p>
Data for "The effect of a weak asthenospheric layer on surface kinematics, subduction dynamics and slab morphology in the lower mantle"
<p>Dataset associated with the paper entitled "The effect of a weak asthenospheric layer on surface kinematics, subduction dynamics and slab morphology in the lower mantle" by Cerpa, N. G., Sigloch, K., Garel, F., Heuret, A., Davies, D. R., and Mihalynuk, M.</p> <p>Please, contact Nestor Cerpa (nestor.cerpa@umontpellier.fr) for additional information</p>
Dataset for High-resolution mantle flow models reveal importance of plate boundary geometry and slab pull forces on generating tectonic plate motions
<p>This repository contains the plugin and dataset used to setup models in the manuscript: "High-resolution mantle flow models reveal importance of plate boundary geometry and slab pull forces on generating tectonic plate motions".</p> <p>The material model plugin used in our models is in the "plugins" folder. The "models" folder contains the reference input parameter file described in the paper. All other model configurations shown in the paper can be obtained by modifying this parameter file. The input files used to set up the models are in the respective folder. Additionally, the Jupyter notebook used to compute residuals of our models is provided in the "scripts" folder.</p> <p> </p>
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DANDI Archive for NWB datasets
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International Brain Laboratory public data
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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.