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751 results for “geology”

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zenodo36/100

Truth Tables for consistency-checking 3D geological models

<p>The Microsoft Excel and PDF representations of the Truth Tables and geo-feature relation exampels&nbsp; are provided as supplementary information to the GMD publication:&nbsp;</p> <p><strong>Consistency-Checking 3D Geological Models</strong></p> <p><strong>Marion N. Parquer, Eric A. de Kemp, Boyan Brodaric and Michael J. Hillier</strong></p> <p>&nbsp;</p>

openOct 2024View details →
zenodo36/100

Applied Geophysics - Magnetic Anomaly Data Mosaic of the Socorro-Guaxupé Geological Area (Brazil)

<p>The Socorro-Guaxup&eacute; area is a complex structural environment formed during Proterozoic times, associated with the formation of the Gondwana Supercontinent. The notable magnetic signatures of these geological areas were selected for an Applied Geophysical project for undergraduates in the Geology Course at the University of S&atilde;o Paulo in 2024.</p> <p>This grid mosaic encompasses airborne magnetic data from areas 15, 14, 7, and 2 of the CODEMIG repository (<a href="http://www.codemig.com.br/" target="_new" rel="noopener">http://www.codemig.com.br/</a>) as well as data from areas 1105, 1117, 1039, 4099, 4112, and 4210 from the Geological Survey of Brazil (SGB-CPRM). The surveys were gridded with cell sizes of 1/4 of the flight line spacing, using the minimum curvature method. Additionally, they were continued to a nominal altitude of 700 m for decreasing noise signal, due to the variable spatial resolution and acquisition techniques. Grid stitching was performed using pairs of grids, with the stitching method implemented in Oasis Montaj software. The locations of all surveys are presented in the figure "socorro-guaxupe_surveys.tif."</p> <p>We would like to thank the team at the Laboratory for Research in Applied Geophysics (LPGA) and the professors from the Rio de Janeiro State University (UERJ) and GeoAtlantico Institute for their technical support in assembling this data.</p> <p>This study was financed in part by the Coordena&ccedil;&atilde;o de Aperfei&ccedil;oamento de Pessoal de N&iacute;vel Superior - Brasil (CAPES) - Finance Code 001 (L. Szameitat 88887.798323/2022-00)</p> <p>&nbsp;</p>

opencc-by-4.0Oct 2024View details →
zenodo36/100

Dataset of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars

<p>This dataset contains the original data and crater counting data&nbsp;of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars.</p>

opencc-by-4.0Jun 2021View details →
zenodo36/100

FIG. 12 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 12. Looking south toward Red Rum (arrow) at the intermediate white beds of Zos Canyon.

opencc-by-4.0Feb 2016View details →
zenodo36/100

FIG. 13 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 13. The Red Rum sublocality, looking west-southwest.

opencc-by-4.0Feb 2016View details →
zenodo36/100

FIG. 14 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 14. Looking northwest from the Red Rum sublocality toward the discovery site (arrow).

opencc-by-4.0Feb 2016View details →
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FIG. 11 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 11. Looking south at the basalmost fluvial red sands at Zos Canyon.

opencc-by-4.0Feb 2016View details →
zenodo36/100

FIG. 7 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 7. Ventral view of the preserved dorsal vertebrae of IGM 100/3181. Anterior is to the right.

opencc-by-4.0Feb 2016View details →
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FIG. 5 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 5. The radius (top) and ulna (bottom) of IGM 100/3181.

opencc-by-4.0Feb 2016View details →
zenodo36/100

FIG. 2. IGM 100 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 2. IGM 100/3181, a partial skeleton of Haya griva.

opencc-by-4.0Feb 2016View details →
zenodo36/100

Fig. 14 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 14. Holotype female of Jerseucoila plesiosoma Liu and Engel, new genus and species (NJ-1006).

opencc-by-4.0Sep 2007View details →
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Fig. 19 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 19. Photomicrograph of holotype female of Kinseycynips succinea (Kinsey).

opencc-by-4.0Sep 2007View details →
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Fig. 2 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 2. Holotype female of Protimaspis costalis Kinsey (ROM).

opencc-by-4.0Sep 2007View details →
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Fig. 18 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 18. Holotype male of Tanaoknemus ecarinatus Liu and Engel, new genus and species (CAS-78).

opencc-by-4.0Sep 2007View details →
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Fig. 8 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 8. Holotype female of Goerania petiolata Liu and Engel, new genus and species (CAS).

opencc-by-4.0Sep 2007View details →
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Fig. 10 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 10. Holotype male of Micropresbyteria caputipressa Liu and Engel, new genus and species (RTMP-

opencc-by-4.0Sep 2007View details →
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Fig. 16 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 16. Holotype female of Syneucoila magnifica Liu and Engel, new genus and species (NJ-1075).

opencc-by-4.0Sep 2007View details →
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Fig. 6 in Phylogeny and Geological History of the Cynipoid Wasps (Hymenoptera: Cynipoidea)

Fig. 6. Holotype female of Proliopteron redactus Liu and Engel, new genus and species (CAS-409).

opencc-by-4.0Sep 2007View details →
zenodo36/100

Text-fig. 4. continued. in Late Miocene (Early Turolian) Vertebrate Faunas And Associated Biotic Record Of The Northern Caucasus: Geology, Taxonomy, Palaeoenvironment, Biochronology

Text-fig. 4. continued.

opencc-by-4.0Dec 2017View details →
dryad36/100

Data from: Bedrock geological map predictions for Phanerozoic fossil occurrences

<p>This is the supplementary data repository of the <em>Paleobiology</em> paper titled <em>Bedrock Geological Map Predictions for Phanerozoic Fossil Occurrences</em>. Geographically-explicit, taxonomically resolved fossil occurrences are necessary for reconstructing macroevolutionary patterns and for testing a wide range of hypotheses in the Earth and life sciences. Heterogeneity in the spatial and temporal distribution of fossil occurrences in the Paleobiology Database (PBDB) is attributable to several different factors, including turnover among biological communities, socioeconomic disparities in the intensity of paleontological research, and geological controls on the distribution and fossil yield of sedimentary deposits. Here we use the intersection of global geologic map data from Macrostrat and fossil collections in the PBDB to assess the extent to which the potentially fossil-bearing, surface-expressed sedimentary record has yielded fossil occurrences. We find a significant and moderately strong positive correlation between geologic map area and the number of fossil occurrences. This correlation is consistent regardless of map unit age and binning protocol, except at period level; the Neogene and Quaternary have non-marine map units covering large areas and yielding fewer occurrences than expected. The sedimentary record of North America and Europe yields significantly more fossil occurrences per sedimentary area than similarly-aged deposits in most of the rest of the world. However, geographic differences in area and age of sedimentary deposits lead to regionally different expectations for fossil occurrences. Using the sampling of surface-expressed sedimentary units in North America and Europe as a predictor for what might be recoverable from the surface-expressed sedimentary deposits of other regions, we find that the rest of the globe is approximately 45% as well sampled in the PBDB. Using age and area of bedrock and sampling in North America and Europe as a basis for prediction, we estimate that over 639 thousand occurrences from outside of these regions would need to be added to the PBDB to achieve global geological parity in sampling. In general, new terrestrial fossil occurrences are expected to have the greatest impact on macroevolutionary patterns. </p>

opencc-zeroDec 2022View details →

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Allen Brain Atlas

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Last verified 2026-04-30Open record

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.

dandi-nwb
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Last verified 2026-04-30Open record

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.

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Last verified 2026-04-29Open record

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.

openneuro
neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record