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215 results for “Slab”
Kildreelig Cross-inscribed Slab 1
Cross-inscribed slab found in the interior of the 6/7th century monastic site at Kildreelig Co.Kerry. It is one of a pair of such slabs at the site, the other located outside the surrounding enclosure wall. Source: Objaverse 1.0 / Sketchfab
Enniskeen - Cross Slab - Inscribed Stone V2
This is a rescanned model the the Enniskeen Cross Slab discovered by Brian from Moybologue. Source: Objaverse 1.0 / Sketchfab
Kildreelig Early Medieval Cross-inscribed slab
One of two cross-inscribed slabs found at the monastic site of Kildreelig. This one is located outside the main enclosure on top of a leacht (possible alter or reliquary). Source: Objaverse 1.0 / Sketchfab
A weak subducting slab at intermediate depths below northeast Japan
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Data from: Ongoing India-Eurasia collision predominantly driven by Sumatra-Java slab pull
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Udayagiri उदयगिरि (Madhya Pradesh). Slab with zodiac imagery.
<p>Udayagiri उदयगिरि (Madhya Pradesh). Slab with zodiac imagery, early fifth century CE. Now Archaeological Museum, Gwalior.</p>
Supplementary Material to "Comparison of equilibrium climate sensitivity estimates from slab ocean, 150-year, and longer simulations"
<p>This is supplementary data for Dunne, J. P., et al. (2020). Comparison of equilibrium climate sensitivity estimates from slab ocean, 150-year, and longer simulations. Geophysical Research Letters. 2020GL088852R. Data in this repository can be unpacked and the files are in the form- NetCDF and matlab files, along with a README. </p> <p>Model data for global average values of net top of the atmosphere radiative balance (W m-2) and 2m air temperature (degrees celsius) for preindustrial control and 4x abrupt CO2 simulations for a variety of models used in LongRunMIP, CMIP5, and CMIP6, as well as scripts used to calculate equilibrium climate sensitivity from these simulations. </p> <p> </p>
Calcium stable isotopes of Tonga and Mariana arc lavas and implications for slab fluid-mediated carbonate transfer in subduction zones
<p>The Table 1 shows Ca isotopes and selected major and trace element compositions of the Tonga rear arc and Mariana arc lavas.</p> <p>Supporting imformation includ Figure S1 and Table S1</p> <p>Figure S1 shows the δ<sup>44/42</sup>Ca‰ versus δ<sup>43/42</sup>Ca‰ in all samples and reference materials measured by Nu Plasma 1700 MC-ICP-MS in GPMR.</p> <p>Table S1 lists the major and trace element contents of NW Rota-1 and Esmeralda Bank samples from Mariana arc. Major elements are tested on board and trace elements are measured by ICP-MS in GPMR.</p>
Database of wide beams and slabs under concentrated loads failing in different shear failure modes
<p>This database includes information about loading, geometry, failure loads, and failure modes of slabs under concentrated loads under different support conditions.</p>
Field-based evidence for intra-slab high-permeability channel formation at eclogite-facies conditions during subduction
<p>Bulk rock analysis of metamorphic rock samples (major and trace element)</p>
Slab metamorphism and interface earthquakes in Peru: implications for along-strike fluid content and seismotectonic variation
<p>Evidenced by a typically shallow subducted thick mid-ocean ridge basalt (MORB) layer that dominates the subducting Nazca plate and a significant lack of arc magmatism, the Peruvian megathrust remain enigmatic in thermal regime and petrological metamorphism. Thermally controlled slab dehydration in the incoming plate may facilitate fluids release and migration which possibly causes fault instability and seismic and aseismic slips. We find that (1) the eclogitization of the MORB layer and the harzburgitization of the ultramafic layer, and the subsequent dehydration embrittlement probably affect interface seismicity in Peru; (2) the subduction of the Nazca Ridge separates southern Peru from north-central Peru, leading to a MORB-dominant oceanic lithosphere beneath Peru associated with an aseismic interface at depth and a lack of arc magmatism; (3) slab dehydration of >0.01 wt%/km accompanied by temperatures of 300-600°C possibly affect the occurrence of earthquakes and slips distributed on the hydrated interface. The along-strike fluid content variation possibly interprets the forearc seismotectonic segmentation associated with pore fluid pressure variation on megathrusts.</p>
Inish Shark - Cross Slab - 10E0399 CL 009
Source: Objaverse 1.0 / Sketchfab
Formaston Class II Pictish Cross Slab, Aboyne
Formaston 1 (St Adomnan), Aboyne, Aberdeenshire, Pictish cross-slab with ogham inscription. Measurements: H 1.12m, W 0.43m, D 0.12m Class II symbol stone bearing mirror, interlace-filled cross-shaft and incised Ogham inscription Place of discovery: NJ 5412 0014 Present location: Victory Hall, Aboyne Found lying in the kirkyard at Formaston before 1874 and moved to the grounds of Aboyne Castle by 1883. It was taken to Inverurie Museum in 1974 and thence to the Victory Hall, Aboyne. The outer line of ogham runs along the roll moulding on the edge of the slab. The oghams are in Irish script and language and include the Pictish names Nehht and Talorc. Date: eighth or ninth century. The slab is in a protective glass case in Victory Hall, Aboyne which makes 3D modelling difficult and it was only possible to model front face. Canmore ID 17507 Source: Objaverse 1.0 / Sketchfab
Inis Gé Medieval Cross Slab
There is not much information on this stone cross slab. However, at some point it was moved from an original context and placed on a concrete slab. The date is also unknown, but it is generally accepted as a medieval cross slab. Irish monks lived on the island between the sixth and 10th century producing purple dye. The stone may be from this period. View in Matcap to view the designs in greater detail. Source: Objaverse 1.0 / Sketchfab
The portcullis slab nub of the Great Pyramid
Original by @homomegalithic1 on Twitter Source: Objaverse 1.0 / Sketchfab
Pictish Slab (later re-use) Meigle Museum, Angus
This elaborately decorated Pictish cross slab was originally carved with cup and ring marks, some of which are just visible at the base of the slab. The others have been set into concrete but are visible on a cast, see: https://sketchfab.com/3d-models/pictish-stone-cast-meigle-museum-angus-c720ea560dfb43fe8bc3a4f8ae010776. For more information, see: https://www.rockart.scot/rock-art-database/?scrapToolsaction=datatools:panel&id=C639207A-3A8C-4F4F-980C282E00102B6B and https://www.rockart.scot/rock-art-database/?scrapToolsaction=datatools:panel&id=4CABFF29-C6EB-427F-961BE1917197FF44 Accreditation: ScRAP ©HES. Source: Objaverse 1.0 / Sketchfab
Elgin Cross Slab
Pictish Cross Slab, at Elgin Cathedral Source: Objaverse 1.0 / Sketchfab
TRUST 3D Dust RT Slab Benchmark Data
<p>Output global SEDs and images at selected wavelengths for the Slab benchmark of the TRUST collaboration. TRUST is a suite of benchmarks for 3D dust radiative transfer codes in astronomy. </p> <p>Paper describing the TRUST Slab benchmark is Gordon et al. (2017, A&A, 603, 114; http://adsabs.harvard.edu/abs/2017A&A...603A.114G)</p> <p>More details on TRUST at http://ipag.osug.fr/RT13/RTTRUST/.</p> <p>Code to make plots using this data at: https://github.com/karllark/trust_slab</p>
Pictish Cross Slab, East Mainland, Orkney
The front face of a Pictish cross slab modelled moments after the stone was lifted and the cross revealed for the first time. The face has not been cleaned and the design it partly concealed by adhering soil, but the form of the cross and the S-dragon to the bottom left are clear. More detail will be visible once the face has been cleaned and conserved. The stone measures 0.85m+ long by 0.55m wide and 0.09m thick. A 3d model rear face of the stone can be viewed here: https://skfb.ly/UQKA This cross probably dates from the 8th century AD. Scan by Dr Hugo Anderson-Whymark, 13th October 2016. Source: Objaverse 1.0 / Sketchfab
GRANITE SLAB - EASTERN GRAY™
Source: Objaverse 1.0 / Sketchfab
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