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96 results for “dolomite”
The Glaciers of the Dolomites: last 40 years of melting
<p><strong>This dataset refers to: </strong></p> <p>Securo, A., Del Gobbo, C., Baccolo, G., Barbante, C., Citterio, M., De Blasi, F., Marcer, M., Valt, M., and Colucci, R. R.: The Glaciers of the Dolomites: last 40 years of melting, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2024-1357, 2024.</p> <p>Read more here: <a href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1357/">https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1357/</a></p> <p>The study presents a multi-decadal (1980s-2023) estimation of surface elevation change and geodetic mass balance of the current mountain glaciers present in the area. Calculations are based on geodetic data: high resolution and accuracy is obtained with unmanned aerial vehicle (UAV) Structure from Motion (SfM) and airborne Light Detection and Ranging (LiDAR), from 2010 to 2023. SfM on historical aerial imagery is used for previous decades.</p> <p><strong>The dataset contains:</strong></p> <ul> <li>1-band raster files (.tif) with the M3C2 (Multi Scale Model to Model Cloud Comparison) distance calculations from all mountain glaciers of the Dolomites, computed on common glacier area between the two periods. File names are as following: "AreaID_glaciername_year1_year2.tif"<br>SR<em> Monte Mario / Italy zone 2 - EPSG:3004</em></li> <li>Geopackage (.gpkg) files with glaciers area during different periods. Polygon have the following attributes: Area ID, Glacier name, CGI-ID (Comitato Glaciologico Italiano), RGI-ID (Randoph Glacier Inventory), Area, Year.<br>SR <em>WGS84 - EPSG: 4326</em></li> </ul> <p><strong>Additional 3D models of the Dolomites Glaciers in 2023 can be found here: <a title="Sketchfab Collection" href="https://skfb.ly/oRtOW" target="_blank" rel="noopener">Sketchfab</a></strong></p> <p><strong>Full file list:</strong></p> <p>"1_Popera_2010_2014.tif"<br>"1_Popera_Alto_1992_2010.tif"<br>"1_Popera_Alto_2010_2023.tif"<br>"1_Popera_Alto_2014_2023.tif"<br>"1_Popera_Pensile_1992_2010.tif"<br>"1_Popera_Pensile_2010_2023.tif"<br>"1_Popera_Pensile_2014_2023.tif"<br>"2_Cristallo_1992_2010.tif"<br>"2_Cristallo_2010_2014.tif"<br>"2_Cristallo_2010_2023.tif"<br>"2_Cristallo_2014_2023.tif"<br>"3_Sorapiss_Occidentale_1980_2010.tif"<br>"3_Sorapiss_Occidentale_2010_2014.tif"<br>"3_Sorapiss_Occidentale_2010_2023.tif"<br>"3_Sorapiss_Occidentale_2014_2023.tif"<br>"4_Antelao_2010_2014.tif"<br>"4_Antelao_Inferiore_1982_2010.tif"<br>"4_Antelao_Inferiore_2010_2023.tif"<br>"4_Antelao_Inferiore_2014_2023.tif"<br>"4_Antelao_Superiore_1982_2010.tif"<br>"4_Antelao_Superiore_2010_2023.tif"<br>"4_Antelao_Superiore_2014_2023.tif"<br>"5_Marmolada_1982_2010.tif"<br>"5_Marmolada_2010_2014.tif"<br>"5_Marmolada_2010_2023.tif"<br>"5_Marmolada_2014_2023.tif"<br>"6_Fradusta_1982_2010.tif"<br>"6_Fradusta_2010_2014.tif"<br>"6_Fradusta_2010_2023.tif"<br>"6_Fradusta_2014_2023.tif"<br>"6_Travignolo_1982_2010.tif"<br>"6_Travignolo_2010_2014.tif"<br>"6_Travignolo_2010_2023.tif"<br>"6_Travignolo_2014_2023.tif"</p> <p>"area_dolomites_glaciers.gpkg"<br>"area_dolomites_glaciers_1980s_1990s.gpkg"<br>"area_dolomites_glaciers_2010.gpkg"<br>"area_dolomites_glaciers_2023.gpkg"</p>
Fig. 9 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 9. Neritariid gastropods Dentineritaria neritina (Münster, 1841) from Lago Antorno (A) and Misurina Landslide (B, C), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12801, in apertural (A1) and apical (A2) views; A3, end of smooth larval shell well visible in oblique lateral view. B. PZO 12683, in apertural (B1) and abapertural (B2) views. C. PZO 12684 in apical view.
Impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, the Dolomites, northern Italy)_DATASET
<p>The datasets (original field photographs, drone images and finite-element modelling algorithms and results) presented here are drawn from the extensive fieldwork, and finite-element modelling of the impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, the Dolomites, northern Italy) by the author(s). These datasets show different rock units in the Latemar platform riddled with diverse structural elements, including fractures (veins, joints, faults) and stylolites, and the results of the impact of the modelled far-field stresses at (i) subsidence deformation from the NW–SE and (ii) Alpine deformation from N–S. All of which increased the overall fracture aperture and permeability of the studied carbonate platform. </p> <p>In addition, the datasets are part of the paper titled "<strong>Impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, the Dolomites, northern Italy)</strong>"<strong>, </strong>published<strong> </strong>in the Solid Earth Journal. </p> <p>The drone images are taken with DJI Phantom 4® and processed using Agisoft PhotoScan® - a photogrammetry tool. The workflow in processing the drone images is publicly available in the published work of Bisdom et al. (2017).</p>
Figure 1 in Insecticidal effect of diatomaceous earth and dolomite powder against Corn weevil Sitophilus zeamais Motschulsky, 1855 (Coleoptera: Curculionidae)
Figure 1. Sitophilus zeamais adults observed using Zeiss stereo-microscope. (A) Dorsal view, (B) Ventral view, and (C) Side view. H: Head, T: Thorax, Ab: Abdomen, R: Rostrum, L: Legs.
Figure 4 in Insecticidal effect of diatomaceous earth and dolomite powder against Corn weevil Sitophilus zeamais Motschulsky, 1855 (Coleoptera: Curculionidae)
Figure 4. Pictures of Sitophilus zeamais exposed to inert dusts taken by scanning electron microscopy (SEM). A. Rostrum (R) of insect exposed to dolomite powder: sensilla (S). Bar = 50 µm. B. Dorsal view of insect exposed to diatomaceous earth: trichoid sensilla (Se), sensilla (S), antenna (A), rostrum (R). Bar = 200 µm. C. Sensilla of insect exposed to dolomite powder. Bar = 5 µm. D. Antenna (A) of insect exposed to diatomaceous earth: trichoid sensilla (Se), sensilla (S). Bar = 50 µm. E. Antenna (A) of insect exposed to dolomite powder: trichoid sensilla (Se), sensilla (S). Bar = 20 µm.
FIGURE 7 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 7. Maximum Likelihood tree of Sphaleroptera orientana.
FIGURE 2 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 2. Sphaleroptera orientana meridionalis sp. nov. holotype, labial palpus.
FIGURE 1 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 1. Sphaleroptera orientana meridionalis sp. nov. holotype, male, dorsal habitus.
FIGURE 4 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 4. Sphaleroptera orientana meridionalis sp. nov. paratype, female, dorsal view.
FIGURE 5 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 5. Sphaleroptera orientana meridionalis sp. nov. paratype, labial palpus.
Figure 5 from: Francesconi L, Conti M, Gheza G, Martellos S, Nimis PL, Vallese C, Nascimbene J (2024) The Dolichens database: the lichen biota of the Dolomites. MycoKeys 103: 25-35. https://doi.org/10.3897/mycokeys.103.115462
Figure 5 Lichen occurrences of the Dolichens dataset per year.
Figure 4 in Oribatid mites (Acari: Oribatida) from the Sella massif (Dolomites, Trentino, Italy) with description of Trichoribates valeriae n. sp. (Ceratozetidae)
Figure 4 Trichoribates valeriaen. sp., adult: lateral view (legs not shown). Scale bar 100 µm.
Effects of Zeolite + Dolomite on Performance and Acidosis
ClinicalTrials.gov study NCT01831492. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Elastic properties of Dolomite at High Pressure and Temperature
<p>It's the elasticity of dolomite at mantle conditions.</p>
Dolomit
<u>Source</u>: Europeana <br><u>4DCity URL</u>: <a href="https://4dcity.org/imgupload/1652249409.1981.jpg">https://4dcity.org/imgupload/1652249409.1981.jpg</a> <br><u>Original Image URL</u>: <a href="https://api.europeana.eu/thumbnail/v2/url.json?uri=http%3A%2F%2Fcoll.mfn-berlin.de%2Fimg%2FMFN_PET_2010_02556__et_Dolomit.jpg&type=IMAGE">https://api.europeana.eu/thumbnail/v2/url.json?uri=http%3A%2F%2Fcoll.mfn-berlin.de%2Fimg%2FMFN_PET_2010_02556__et_Dolomit.jpg&type=IMAGE</a> <br><br><u>Image-Metadata:</u><br>Filename: 1652249409.1981.jpg<br>Image Dimensions: 400x271<br>Megapixels: 0.11 MP<br>Filesize: 20.06 KB<br>
FIGURE 9 in Description of Sphaleroptera orientana meridionalis subs. n. (Lepidoptera: Tortricidae: Cnephasiini) from the Pale di San Martino Mountain plateau (Dolomites, NE Italy)
FIGURE 9. Pale di San Martino plateau, locus typicus of Sphaleroptera orientana meridionalis sp. nov.
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OpenNeuro
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