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215 results for “Slab”
Cross-inscribed slab
This cross-inscribed slab was captured for demo during class on 02/02/2013 and processed using Autodesk 123DCatch. The book was employed to support the slab. Source: Objaverse 1.0 / Sketchfab
Loch Kinord 9th Century Cross Slab
Canmore ID 33981 NO 4400 9978 Loch Kinord, Dinnet, Deeside, Scotland. Class III Pictish Stone. In the mid nineteenth century this pink granite stone, H 1.91m, W 0.94m, D 0.31m, stood 'on an eminence' on the north bank of Loch Kinord, but later that century it was taken to the grounds of Aboyne Castle and set up in a 'small oak plantation' (NO 5250 9898). In 1959 it was returned to approximately its original site beside Loch Kinord. Roughly kite-shaped, this eigth or ninth century slab is carved in relief on one broad face with an elaborate ringed cross, which occupies most of the available space. The cross is outlined by a roll moulding, which extends into a spiral at each corner of the arm terminals and into a semi-spiral at the base of the shaft. The circular arm-pits are closed by arcs of a ring. The entire cross is filled with continuous interlace, which in the side arms conveys an impression of triquetra knots and in the upper arm forms four ring knots. Source: Objaverse 1.0 / Sketchfab
Inish Shark - Cross Slab - 10E0399 CL 006AO
Source: Objaverse 1.0 / Sketchfab
Drum slab from the Amaravati stupa
A drum slab carved in limestone with the four events related to the Buddha's birth: Māyādevī's Dream (top right); the Interpretation of the Dream attended by the dīkpāla-s (top left); the Birth of the Buddha attended again by the dīkpāla-s (bottom right); the Presentation of the Buddha to the caitya of the Śākyas (bottom left). Height: 157.5 centimetres Width: 96.25 centimetres Thickness: 14 centimetres COL: [RRI1193](http://www.britishmuseum.org/research/collection_online/collection_object_details.aspx?objectId=251183&partId=1) Model by Daniel Pett, created from 330 photographs taken with a Sony A6000 through the glass case, assembled in Photoscan Pro. Source: Objaverse 1.0 / Sketchfab
Retention of water in subducted slabs under core-mantle boundary conditions
Open the record for dataset details and reuse information.
Supplementary Data Sets for Machine Learning Tracks the Role of Slab-Derived Fluids in Large Igneous Province/CUGBZL
<p>Supplementary Dataset S1: All data collcted from both the GEOROC database and recent literature published in Chinese and English journals and books.<span></span></p> <p>Supplementary Dataset S2: Data after cleaning.</p> <p>Supplementary Dataset S3: Prediction results.</p>
Low thermal conductivity of hydrous phase D leads to a self-preservation effect within a subducting slab
<p>This repository contains experimental data on the thermal conductivity of hydrous phase D mineral at high pressure and temperature. This dataset is presented in a manuscript submitted by Wen-Pin Hsieh, Enrico Marzotto, Takayuki Ishii, Leonid Dubrovinsky, Alena A. Aslandukova, Giacomo Criniti, Yi-Chi Tsao, Chun-Hung Lin, Jun Tsuchiya, and Eiji Ohtani entitled:</p> <p>Low thermal conductivity of hydrous phase D leads to a self-preservation effect within a subducting slab</p>
Supporting information for "Amorphous Mn2SiO4: A potential manganese phase in the stagnant slab"
<p>This is the supplementary file for the article "Amorphous Mn2SiO4: A potential manganese phase in the stagnant slab". It includes 5 supplementary texts, 7 figures, and 6 tables.</p> <p>Supplementary texts describe experimental methods, single-crystal X-ray diffraction results, and high-pressure Raman spectra results.</p> <p>Figures show the experimental PT path, crystal structure of tephroite, normalized unit-cell parameters as a function of pressure, pressure independence of polyhedron volume and averaged bond length, pressure dependence of the Raman-active modes for tephroite, amorphous transformation pressure of end-member olivine.</p> <p>Tables describe chemical compositions of tephroite, lattice parameters and unit-cell volumes of tephroite, structure refinement details, best-fit volumetric and linear BM3 parameters, frequency of Raman modes of tephroite.</p>
Elastic Anomalies across the α-β Phase Transition in Orthopyroxene: Implication for the Metastable Wedge in the Cold Subduction Slab
<p>Here are the expeirmental data</p>
A lower mantle slab below the East Asia margin constrained by seismic waveform complexity
<p>This dataset consists of two parts: the waveforms of four events and the calculated MPD data for three of them. The waveforms for each event are recorded at the stations along the 2D profile. While the MPD data contains all the stations from the China National Seismic Network. </p>
The 2021 and 2022 Fukushima-Oki Earthquake Doublet: Reactivations of the Bending-Related Faults Inside the Japan Trench Subducting Slab
<p>The strong-motion (K-NET, KiK-net and S-net) waveforms and teleseismic <em>P</em> waves that were processed and used in the joint inversions of the 2021 <em>M</em><sub>w</sub>7.1 and 2022 <em>M</em><sub>w</sub> 7.3 Fukushima-Oki earthquakes are included in this repository.</p>
Distance Slab from the Antonine Wall (A.1942.18)
Rectangular Roman distance slab from the Antonine Wall, made of local buff sandstone, and dug up in 1803 on the land of East Millichen (formerly Low Millochan) Farm, around 100m south of the line of the Antonine Wall (NS 573 720). The slab was subsequently built into the wall of a dovecot near Strathleven House in Dumbarton. The incised Latin inscription on the slab testifies to the completion of 3666 and a half paces of the Antonine Wall, between Summerston and Castlehill, by a detachment of the Sixth Legion (Sixth Victrix). The inscription is framed by moulding carved in relief, flanked by peltae, the horns of which terminated in griffin-heads and the central projections in rosettes (now much worn). The slab is fractured vertically across the inscription, the top right and bottom left-hand corners are missing, and the stone is generally very weathered. Source: Objaverse 1.0 / Sketchfab
Pictish cross slab fragment, 7th-11th Century.
Sandstone. Found at Easter Clunie Farm Courtesy of David Baird. Source: Objaverse 1.0 / Sketchfab
Pictish Cross Slab No 2, St Fergus', Dyce
The Class II stone is sculpted on one face with a Celtic cross ornamented with a central boss of spiral work and elsewhere with interlace. Beside it, and below the shaft, are the crescent and V-rod, mirror case, double disc and Z-rod and the triple ring symbols. This stone also has an ogham inscription on the right side which reads '(eottassarrhetoddeddots) maqq Rogoddadd', although this is difficult to interpret. Canmore 19466 Source: Objaverse 1.0 / Sketchfab
St Orland's Cross Slab
https://canmore.org.uk/site/33868/cossans-st-orlands-stone Source: Objaverse 1.0 / Sketchfab
Pictish Cross Slab, Orkney
Rear face of a recently discovered Pictish cross slab found in East Mainland, Orkney Scan by Dr Hugo Anderson-Whymark, 20th October 2016. Source: Objaverse 1.0 / Sketchfab
Nicosia, Cyprus. Tomb slab dated 1558
<p>Nicosia, Cyprus. Tomb slab dated 1558. Now I the Medieval Museum of Cyprus, Castle of Lemesos.</p>
The Role of the Overriding Plate and Mantle Viscosity Structure on Deep Slab Morphology
<p>Movies of viscosity and temperature for V1-V3 with a continental and oceanic overriding plate for the manuscript </p>
Fore-arc metasomatism by hybrid slab fluids during subduction initiation: Sr–Mg–Ca isotopes of rodingite, western Yarlung Zangbo suture zone
<p> Subduction zone metasomatism is critical for Earth’s material exchanges, yet understanding slab dehydration, particularly deserpentinization beneath fore-arcs, remains challenging. Here, we present Sr–Mg–Ca isotopic data for the Purang rodingites in the western Yarlung-Zangbo suture zone (YZSZ). These rodingites, dominated by amphibolite- to greenschist-facies minerals like tremolite, magnesiohornblende, and chlorite, exhibit cumulate textures and rare earth element patterns resembling troctolites or gabbronorites, presumably formed beneath a seafloor spreading center. The rodingites are enriched in large ion lithophile elements and depleted in high field strength elements. They show higher initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.7067–0.7075) and elevated δ<sup>26</sup>Mg values (–0.22 ± 0.07‰ to –0.13 ± 0.02‰) compared to pristine oceanic basalts, while their δ<sup>44/40</sup>Ca values (0.72 ± 0.02‰ to 0.87 ± 0.03‰) correspond to mid-ocean ridge basalts (MORB). These features imply fore-arc mantle metasomatism of an original MOR-derived protolith at <40 km slab depth, driven by Sr- and Mg-rich fluids from clay-rich sediments and serpentinitized mantle, respectively. The measured Sr and Mg isotope compositions can be reproduced by mixing a MORB-like protolith with hybrid fluids derived from 70–30% clays and 30–70% serpentinites, with a fluid-to-rock ratio of approximately 1:3–1:5. Combined with studies on YZSZ metamorphic soles, we propose this metasomatism occurred during incipient subduction of the Neo-Tethys oceanic rocks. Our studies highlight the significance of deserpentinization at shallow fore-arc mantle settings during subduction initiation and suggest that subducting slabs exhibit more varied dehydration characteristics than previously recognized.</p>
Modeling Anisotropic Signature of Slab-induced Mantle Plumes from Thermochemical Piles in the Lower Mantle
<p># Modeling Anisotropic Signature of Slab-induced Mantle Plumes from Thermochemical Piles in the Lower Mantle: Data</p> <p>This repository accompanies the paper</p> <p>```<br>Roy P., Steinberger B., Faccenda M., Pons M.: Modeling Anisotropic Signature of Slab-induced Mantle Plumes from Thermochemical Piles in the Lower Mantle</p> <p>```</p> <p>This repository contains the ASPECT data files, input files and the version of ASPECT required to run the geodynamic models. ASPECT data files can be found within /data_package/ASPECT_data_files/<br>ASPECT input files can be found within /data_package/cartesian_models/ASPECT_input_files/<br>The code is found within /data_package/aspect_steinberger_multicomponent_topolayer/</p> <p>It also provides the databases, input files and the version of D-REX_M used in this study.<br>D-REX_M data files can be found within /data_package/D-REX_M_mod/ASPECT_database/<br>D-REX_M input files can be found within /data_package/cartesian_models/ECOMAN_input_files/<br>The D-REX_M code is found within /data_package/D-REX_M_mod/D-REX_M_modified/</p> <p><br>The ASPECT branch that has been used:</p> <p>Branch: steinberger_multicomponent_topolayer<br>ASPECT Version: aspect_steinberger_multicomponent_topolayer</p> <p>```<br>-----------------------------------------------------------------------------<br>This is ASPECT, the Advanced Solver for Problems in Earth's ConvecTion.<br>-- . version 2.5.0-pre (steinberger_multicomponent_topolayer, cf2e084)<br>-- . using deal.II 9.4.0<br>-- . with 32 bit indices and vectorization level 1 (128 bits)<br>-- . using Trilinos 13.2.0<br>-- . using p4est 2.3.2<br>-----------------------------------------------------------------------------<br>```</p>
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Allen Brain Atlas
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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.