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10 results for “partial melting”
An Experimental Investigation of Reactive Melt Channelization in Partially Molten Rocks
<p>Mechanical, microstructural and chemical data from experiments on reactive melt migration. Each zip file contains all data from the specific experiment that were collected (optical images, scanning electron microscope images, microCT reconstructions, electron microprobe data). Master metadata table is provided with all details about the performed experiments. Experiment number corresponds to zip file number. Further information about the dataset is contained in the following publications:</p> <p>Matej Pec, Benjamin K. Holtzman, Mark Zimmerman, David L. Kohlstedt; (2015) Reaction infiltration instabilities in experiments on partially molten mantle rocks. <em><em>Geology</em></em> ; 43 (7): 575–578. doi: <a href="https://doi.org/10.1130/G36611.1">https://doi.org/10.1130/G36611.1</a></p> <p>Matej Pec, Benjamin K. Holtzman, Mark E. Zimmerman, David L. Kohlstedt, (2017) Reaction Infiltration Instabilities in Mantle Rocks: an Experimental Investigation, <em>Journal of Petrology</em>, Volume 58, Issue 5, May 2017, Pages 979–1003, <a href="https://doi.org/10.1093/petrology/egx043">https://doi.org/10.1093/petrology/egx043</a></p> <p>Matej Pec, Benjamin K. Holtzman, Mark E. Zimmerman, David L. Kohlstedt, (submitted) Influence of Lithology on Reactive Melt Flow Channelization: Infiltration Instabilities and Dikes, submitted to<em> Geochemistry, Geophysics, Geosystems</em></p>
Supplementary Material to "Partial melting of amphibole–clinozoisite eclogite at the pressure maximum (eclogite type locality, Eastern Alps, Austria)"
<p><span>Here we briefly describe the supplementary materials for the publication “Partial melting of amphibole–clinozoisite eclogite at the pressure maximum (eclogite type locality, Eastern Alps, Austria)” in the European Journal of Mineralogy, 35(5), 715-735 Schorn, S., Rogowitz, A., & Hauzenberger, C. A. (2023).</span></p>
Uranium-series disequilibria in MORB, revisited: A systematic numerical approach to partial melting of a heterogeneous mantle
<p><span>This directory includes all of the gridded run results for each melting scenario for this paper, organized into approx. 50 supplementary figures with a series of activity ratio diagrams.</span></p>
Partial molar volumes of H2O and CO2 in pyrolite melt
<p>Partial molar volumes of CO<sub>2</sub> and H<sub>2</sub>O in pyrolite melt as a function of pressure at 2000 K, 3000 K, 4000 K and 5000 K. Each file is a text file where the first column is the pressure (units: GPa) and the second column is the partial molar volume of the volatile (units: cm<sup>3</sup>/mol). The partial molar volumes of the volatiles were determined from subtracting the equations of state of volatile-bearing pyrolite melt from the equation of state of volatile-free pyrolite melt.</p>
Large variations of Calcium isotopes in Lutao arc volcanic rocks: Influence of recycled marine carbonate and partial melting
<p>The dataset for the manuscript in preparation: Large variations of Calcium isotopes in Lutao arc volcanic rocks: Influence of recycled marine carbonate and partial melting</p>
Early Partial Melting and Formation of Na-rich Asteroidal Crust from the Albite-rich Achondrite Erg Atouila 001
<p>This is the research data related to the manuscript titled: Early Partial Melting and Formation of Na-rich Asteroidal Crust from the Albite-rich Achondrite Erg Atouila 001,<strong> </strong>including the the petrological and elemental mapping images, and the supplementary materials of the manuscript.</p>
Nesokia is sister to Bandicota and are nested in Rattus phylogenetically, making Rat- tus paraphyletic. Tarsomys, Limnomys, and Diplothrix are also phylogenetically in Rat- tus, and the clade is in need of focused re- vision at the generic level. Nesokia bunnui was originally described as a separate ge-nus, Erythronesokia, because it is morphologically very distinctive from N. indica. Type specimen was destroyed during the Iraq War, and a neotype was recently designated to replace it. Monotypic. Distribution. Tigris and Euphrates river valleys, SE Iraq. Descriptive notes. Head—body 230-260 mm, tail 205-270 mm, ear 18-21 mm, hindfoot 49-58 mm; weight 519 g. The Long-tailed Bandicoot Rat is larger than the Short-tailed Bandicoot Rat (N. indica). Pelage is soft and woolly, interspersed with harsher coarse hair and long black hairs near mid-back. Dorsum is fawn to ocherous red, washed with purple or chestnuton darker individuals. Hairs are basally slate-gray and distally rufous, occasionally with whitish or black tips. Muzzle is drab. Sides arefawn, with gray edge toward venter. Venteris whitish, extending onto cheeks where the same pattern from gray to fawn to dorsal pelage occurs. Feet are large and robust, being light brown and well-furred dorsally. Claws are amber on forefeet and dull brown on hindfeet; pollux is extremely small. Ears are moderately long and brownish, with no hair internally. Tail is ¢.82-104% of head-body length and deep brownish drab, interspersed with visible white hair. Skull is large and robust, similarly to the Short-tailed Bandicoot Rat. Habitat. Marsh and swamp land. Food and Feeding. No information. Breeding. No information. Activity patterns. The Long-tailed Bandicoot Rat is terrestrial, although it isfound in swampy and marshy areas and is probably amphibious. Movements, Home range and Social organization. No information. Status and Conservation. Classified as Endangered on The IUCN Red List. The Longtailed Bandicoot Rat is apparently rare and is known from very few specimens. Marsh and swamp habitats in which it is found were completely destroyed during the Iraq War by draining, war damage, and agricultural expansion. In recent years, flooding from Tigris and Euphrates rivers and high snow fall and melt haveresulted in partial restoration ofits native habitat, although restoration is not a complete. Populations are now probably highly fragmented. Bibliography. Al-Ansari et al. (2012), Al-Robaae & Felten (1990), Khajuria (1981), Krystufek et al. (2017), Musser & Carleton (2005), Richardson & Hussain (2006), Stuart (2008). in Muridae
Nesokia is sister to Bandicota and are nested in Rattus phylogenetically, making Rat- tus paraphyletic. Tarsomys, Limnomys, and Diplothrix are also phylogenetically in Rat- tus, and the clade is in need of focused re- vision at the generic level. Nesokia bunnui was originally described as a separate ge-nus, Erythronesokia, because it is morphologically very distinctive from N. indica. Type specimen was destroyed during the Iraq War, and a neotype was recently designated to replace it. Monotypic. Distribution. Tigris and Euphrates river valleys, SE Iraq. Descriptive notes. Head—body 230-260 mm, tail 205-270 mm, ear 18-21 mm, hindfoot 49-58 mm; weight 519 g. The Long-tailed Bandicoot Rat is larger than the Short-tailed Bandicoot Rat (N. indica). Pelage is soft and woolly, interspersed with harsher coarse hair and long black hairs near mid-back. Dorsum is fawn to ocherous red, washed with purple or chestnuton darker individuals. Hairs are basally slate-gray and distally rufous, occasionally with whitish or black tips. Muzzle is drab. Sides arefawn, with gray edge toward venter. Venteris whitish, extending onto cheeks where the same pattern from gray to fawn to dorsal pelage occurs. Feet are large and robust, being light brown and well-furred dorsally. Claws are amber on forefeet and dull brown on hindfeet; pollux is extremely small. Ears are moderately long and brownish, with no hair internally. Tail is ¢.82-104% of head-body length and deep brownish drab, interspersed with visible white hair. Skull is large and robust, similarly to the Short-tailed Bandicoot Rat. Habitat. Marsh and swamp land. Food and Feeding. No information. Breeding. No information. Activity patterns. The Long-tailed Bandicoot Rat is terrestrial, although it isfound in swampy and marshy areas and is probably amphibious. Movements, Home range and Social organization. No information. Status and Conservation. Classified as Endangered on The IUCN Red List. The Longtailed Bandicoot Rat is apparently rare and is known from very few specimens. Marsh and swamp habitats in which it is found were completely destroyed during the Iraq War by draining, war damage, and agricultural expansion. In recent years, flooding from Tigris and Euphrates rivers and high snow fall and melt haveresulted in partial restoration ofits native habitat, although restoration is not a complete. Populations are now probably highly fragmented. Bibliography. Al-Ansari et al. (2012), Al-Robaae & Felten (1990), Khajuria (1981), Krystufek et al. (2017), Musser & Carleton (2005), Richardson & Hussain (2006), Stuart (2008).
Mercury's crustal thickness correlates with lateral variations in mantle melt production: Dataset for maps of surface density, degree of partial melting, and crustal thickness
<p>1) DensityGrid.dat = map of density of pore-free surface rocks (Figure 1a)</p> <p>- Units = g/cm3</p> <p>- 720 x 1440 pixels corresponding to 0.25-degree pixels in an equirectangular cylindrical projection with the equator as central parallel.</p> <p>- The first row represents 90 to 89.75 degrees of latitude north; the last row represents 89.75 to 90 degrees of latitude south.</p> <p>- The first column represents 0 to 0.25 degree of longitude; the last column represents 359.75 to 360 degrees of longitude.</p> <p>2) MeltGrid.dat = map of degree of partial melting (Figure S1a)</p> <p>- Units: mass fraction</p> <p>- 720 x 1440 pixels as described above</p> <p>3) CrustalThickness_ModelU0.dat = map of crustal thickness if laterally uniform density, Model U0 (Figure 2a)</p> <p> CrustalThickness_ModelVn.dat = map of crustal thickness if laterally variable density, Model Vn (Figure 2c, Figures S6 to S10)</p> <p>- Units = km</p> <p>- generated with MakeGridDH of SHTOOLS (<a href="https://shtools.github.io/SHTOOLS/">https://shtools.github.io/SHTOOLS/</a>)</p> <p>- 720 x 1440 coordinate points corresponding to 0.25-degree spacing in an equirectangular cylindrical projection with the equator as central parallel.</p> <p>- The first row corresponds to 90 degrees of latitude north; the last row corresponds to 89.75 degrees of latitude south.</p> <p>- The first column corresponds to 0 degree of longitude; the last column corresponds to 359.75 degrees of longitude.</p> <p>Note: Figures refer to the following paper (Geophysical Research Letters, 2020): `Mercury's crustal thickness correlates with lateral variations in mantle melt production’, by M. Beuthe, B. Charlier, O. Namur, A. Rivoldini, and T. Van Hoolst</p>
Early Partial Melting Activity in Asteroids: Insights from Petrogenesis and Chronology of the Albite-rich Achondrite Erg Atouila 001
<p><span>The BSE, elemental mapping images, geochemical and crystallographic data of Erg Atouila 001.</span></p>
Experimental investigation on the transport of sulfide driven by melt-rock reaction in partially molten peridotite
<p>The statistical results of grain size of olivine, clinopyroxene and sulfide droplets in our experiments</p>
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
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.