cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.29885751
title: Surface and subsurface geology of the Hontomín structure, Western Pyrenees

description: A detailed geological study was conducted in the Hontomín area in the western Pyrenees, Northern Spain, focusing on structural characterization by integrating available subsurface data with a newly developed surface geological map. It reveals a relatively simple surface structure, with the Upper Cretaceous generally dipping gently eastward, except at the southern margin, where they are deformed into tight E-W-trending folds. In contrast, the unconformable Cenozoic layers dip only a few degrees southward. However, seismic data interpretation reveals a much more complex subsurface structure. It is dominated by a broad dome, cored by Upper Triassic salt, which has significantly influenced the overlying stratigraphy and structure. Above the salt, the Jurassic and Lower Cretaceous units exhibit moderate folding, a deformation style that is not apparent at the surface. The deep structure is controlled by a major E-W trending thrust fault, which is not clearly expressed at surface except through small-scale, tight folds aligned in the same direction. This study highlights the importance of integrating surface mapping with geophysical data, both for accurately interpreting subsurface geology when planning for CO₂ injection operations.
DOI: 10.6084/m9.figshare.29885751.v1
title: Surface and subsurface geology of the Hontomín structure, Western Pyrenees

description: A detailed geological study was conducted in the Hontomín area in the western Pyrenees, Northern Spain, focusing on structural characterization by integrating available subsurface data with a newly developed surface geological map. It reveals a relatively simple surface structure, with the Upper Cretaceous generally dipping gently eastward, except at the southern margin, where they are deformed into tight E-W-trending folds. In contrast, the unconformable Cenozoic layers dip only a few degrees southward. However, seismic data interpretation reveals a much more complex subsurface structure. It is dominated by a broad dome, cored by Upper Triassic salt, which has significantly influenced the overlying stratigraphy and structure. Above the salt, the Jurassic and Lower Cretaceous units exhibit moderate folding, a deformation style that is not apparent at the surface. The deep structure is controlled by a major E-W trending thrust fault, which is not clearly expressed at surface except through small-scale, tight folds aligned in the same direction. This study highlights the importance of integrating surface mapping with geophysical data, both for accurately interpreting subsurface geology when planning for CO₂ injection operations.
DOI: 10.6084/m9.figshare.30422675
title: Geology of the Bach quadrangle (H15), Mercury

description: Mercury's Bach quadrangle (H15) is the area poleward of 65°S. We mapped this geologically using remote sensing-based observations of surface morphology revealed on MESSENGER data products. This map contributes to a series of quadrangle maps providing geological context forthe ESA-JAXA BepiColombo mission to Mercury. We performed digitisation at ∼1:400,000 scale and final publication scale is 1:3,000,000. There are four morphologically distinct plains units: intercrater, intermediate, smooth, and very smooth. Impact craters cover much of H15's surface. Following convention, we mapped crater materials for all craters ≥20 km, classifying them on the basis of morphological evidence for degradation. We produced two map versions, using a three-class and a five-class crater degradation scheme. We include two geological aspects that have not featured in previous maps of the series, by mapping occurrences of lobate ejecta at craters ≥20 km and depicting the distribution of the south polar permanently shadowed regions.
DOI: 10.6084/m9.figshare.30422675.v2
title: Geology of the Bach quadrangle (H15), Mercury

description: Mercury's Bach quadrangle (H15) is the area poleward of 65°S. We mapped this geologically using remote sensing-based observations of surface morphology revealed on MESSENGER data products. This map contributes to a series of quadrangle maps providing geological context forthe ESA-JAXA BepiColombo mission to Mercury. We performed digitisation at ∼1:400,000 scale and final publication scale is 1:3,000,000. There are four morphologically distinct plains units: intercrater, intermediate, smooth, and very smooth. Impact craters cover much of H15's surface. Following convention, we mapped crater materials for all craters ≥20 km, classifying them on the basis of morphological evidence for degradation. We produced two map versions, using a three-class and a five-class crater degradation scheme. We include two geological aspects that have not featured in previous maps of the series, by mapping occurrences of lobate ejecta at craters ≥20 km and depicting the distribution of the south polar permanently shadowed regions.
DOI: 10.6084/m9.figshare.30422675.v1
title: Geology of the Bach quadrangle (H15), mercury

description: Mercury’s Bach quadrangle (H15) is the areapoleward of 65 °S. We mapped this geologically using remote sensing-basedobservations of surface morphology revealed on MESSENGER data products. Thismap contributes to a series of quadrangle maps providing geological context forthe ESA-JAXA BepiColombo mission to Mercury. We performed digitisation at ∼1:400,000scale and final publication scale is 1:3,000,000. There are four morphologicallydistinct plains units: intercrater, intermediate, smooth, and very smooth.Impact craters cover much of H15’s surface. Following convention, we mappedcrater materials for all craters ≥20 km, classifying them on the basis ofmorphological evidence for degradation. We produced two map versions, using athree-class and a five-class crater degradation scheme. We include twogeological aspects that have not featured in previous maps of the series, bymapping occurrences of lobate ejecta at craters ≥20 km and depicting thedistribution of the south polar permanently shadowed regions.
DOI: 10.6084/m9.figshare.30508963
title: Reconstruction of land cover distribution for mid-twentieth century in Ebro basin

description: The analysis of historical land use and land cover evolution requires available cartography. In this paper, we provided a reconstruction of land cover distribution for mid-twentieth century of part of the Ebro basin. This reconstruction is carried out using three methods: (i) previously available cartographic sources, (ii) land cover reconstruction by data extrapolation in some areas where land cover surface is like other with land cover data availability, and (iii) manual digitization based on 1956–57 orthophotography. As a result, we provide land cover cartography for 71.7% of the study area and the estimated land cover distribution of data for the rest 28.3%. There is a lack of historical land cover data for the Ebro basin We provide a land cover cartography and distribution data of the mid-twentieth century in the upper and middle Ebro basin The reconstruction of land cover data has been made following a mixed methodology based on existing cartography and data contribution, the extrapolation of homogeneous land cover distribution areas and manual digitization
DOI: 10.6084/m9.figshare.30508963.v1
title: Reconstruction of land cover distribution for mid-twentieth century in Ebro basin

description: The analysis of historical land use and land cover evolution requires available cartography. In this paper, we provided a reconstruction of land cover distribution for mid-twentieth century of part of the Ebro basin. This reconstruction is carried out using three methods: (i) previously available cartographic sources, (ii) land cover reconstruction by data extrapolation in some areas where land cover surface is like other with land cover data availability, and (iii) manual digitization based on 1956–57 orthophotography. As a result, we provide land cover cartography for 71.7% of the study area and the estimated land cover distribution of data for the rest 28.3%. There is a lack of historical land cover data for the Ebro basin We provide a land cover cartography and distribution data of the mid-twentieth century in the upper and middle Ebro basin The reconstruction of land cover data has been made following a mixed methodology based on existing cartography and data contribution, the extrapolation of homogeneous land cover distribution areas and manual digitization
DOI: 10.6084/m9.figshare.30508963.v2
title: Reconstruction of land cover distribution for mid-twentieth century in Ebro basin

description: The analysis of historical land use and land cover evolution requires available cartography. In this paper, we provided a reconstruction of land cover distribution for mid-twentieth century of part of the Ebro basin. This reconstruction is carried out using three methods: (i) previously available cartographic sources, (ii) land cover reconstruction by data extrapolation in some areas where land cover surface is like other with land cover data availability, and (iii) manual digitization based on 1956–57 orthophotography. As a result, we provide land cover cartography for 71.7% of the study area and the estimated land cover distribution of data for the rest 28.3%. There is a lack of historical land cover data for the Ebro basin We provide a land cover cartography and distribution data of the mid-twentieth century in the upper and middle Ebro basin The reconstruction of land cover data has been made following a mixed methodology based on existing cartography and data contribution, the extrapolation of homogeneous land cover distribution areas and manual digitization
DOI: 10.6084/m9.figshare.29885763
title: The Jurassic structure of the northern sector of Foligno mountains (Central Italy)

description: This study examines the Jurassic palaeogeography and tectonic evolution of the northern Foligno mountains. A 1:10,000-scale geological survey highlights the impact of Jurassic extensional faulting on depositional environments. Persistent bathymetric differences due to faulting existed as early as the Early Jurassic within the Calcare Massiccio carbonate platform, but fault-bounded structural highs formed only after the platform fragmentation. The main raised structure (Sasso di Pale – Ponte Santa Lucia) can be interpreted as a horst-like feature, bordered by antithetic ESE-WNW faults, with a gently tilted surface affected by sliding processes and edge erosion. The faults reached a total throw of over 500 m already during the Early Jurassic, forming steep escarpments only in part buried by sedimentation. During the Middle and Late Jurassic, these fault scarps protruded 150–200 m above the sea floor, and their prolonged exposure resulted in decompression-related fracturing and block detachments.
DOI: 10.6084/m9.figshare.29885763.v1
title: The Jurassic structure of the northern sector of Foligno mountains (Central Italy)

description: This study examines the Jurassic palaeogeography and tectonic evolution of the northern Foligno mountains. A 1:10,000-scale geological survey highlights the impact of Jurassic extensional faulting on depositional environments. Persistent bathymetric differences due to faulting existed as early as the Early Jurassic within the Calcare Massiccio carbonate platform, but fault-bounded structural highs formed only after the platform fragmentation. The main raised structure (Sasso di Pale – Ponte Santa Lucia) can be interpreted as a horst-like feature, bordered by antithetic ESE-WNW faults, with a gently tilted surface affected by sliding processes and edge erosion. The faults reached a total throw of over 500 m already during the Early Jurassic, forming steep escarpments only in part buried by sedimentation. During the Middle and Late Jurassic, these fault scarps protruded 150–200 m above the sea floor, and their prolonged exposure resulted in decompression-related fracturing and block detachments.
DOI: 10.6084/m9.figshare.29108120
title: Bouguer gravity anomaly in the Colfiorito Quaternary continental basin, northern Apennines, central Italy

description: Gravity anomaly data provides fundamental contributions to the investigation of the geological features at the crustal scale. In this work we present new gravity data acquired over the Quaternary Colfiorito basin in central Italy. After standard correction of such new data, we present the Bouguer anomaly map that we calculate from it. We also attempt a first order modeling of the data by calculating regional and residual field anomalies over the basin and an estimate of the depth to the bedrock beneath the basin infill. The density of gravity stations over the basin improved from less than 1 station per square kilometer in the previously available data, to over 20 stations per square kilometer. This, coupled with the maps of the residual anomaly and of the depth to the bedrock, will likely support a more detailed and reliable investigation of the basin.
DOI: 10.6084/m9.figshare.29108120.v1
title: Bouguer gravity anomaly in the Colfiorito Quaternary continental basin, northern Apennines, central Italy

description: Gravity anomaly data provides fundamental contributions to the investigation of the geological features at the crustal scale. In this work we present new gravity data acquired over the Quaternary Colfiorito basin in central Italy. After standard correction of such new data, we present the Bouguer anomaly map that we calculate from it. We also attempt a first order modeling of the data by calculating regional and residual field anomalies over the basin and an estimate of the depth to the bedrock beneath the basin infill. The density of gravity stations over the basin improved from less than 1 station per square kilometer in the previously available data, to over 20 stations per square kilometer. This, coupled with the maps of the residual anomaly and of the depth to the bedrock, will likely support a more detailed and reliable investigation of the basin.
DOI: 10.6084/m9.figshare.28652550
title: Geotourism of Ignatian Way (Basque Country, Spain)

description: The pilgrimage that Ignatius of Loyola made in 1522 is now a route for religious, sporting and cultural purposes. Its route through the Basque Country (north Spain) has been superimposed on the geological map. The resulting georoute allows us to narrate the alpine geological evolution of the Basque-Cantabrian Basin, from outcrop scale to global tectonics. The path summarizes the geology of the North Iberian margin, from the Iberia-Eurasia plate boundary to the foreland of the Cenozoic Ebro basin. At each stage, the origin of the rocks and their geological context are explained. The resulting brochure has been prepared with freely available information and maps from the geological and tourist public services of the Basque Government. The methodology used can serve as a reference in the development of other georoutes. A georoute brochure of the Ignatian Way across the Basque Country is presented.The maps and geological cross-sections of the Ignatian Way increase the tourist offer: spiritual, cultural, sports and gastronomic.The compiled information is freely available in institutional websites. A georoute brochure of the Ignatian Way across the Basque Country is presented. The maps and geological cross-sections of the Ignatian Way increase the tourist offer: spiritual, cultural, sports and gastronomic. The compiled information is freely available in institutional websites.
DOI: 10.6084/m9.figshare.28652550.v1
title: Geotourism of Ignatian Way (Basque Country, Spain)

description: The pilgrimage that Ignatius of Loyola made in 1522 is now a route for religious, sporting and cultural purposes. Its route through the Basque Country (north Spain) has been superimposed on the geological map. The resulting georoute allows us to narrate the alpine geological evolution of the Basque-Cantabrian Basin, from outcrop scale to global tectonics. The path summarizes the geology of the North Iberian margin, from the Iberia-Eurasia plate boundary to the foreland of the Cenozoic Ebro basin. At each stage, the origin of the rocks and their geological context are explained. The resulting brochure has been prepared with freely available information and maps from the geological and tourist public services of the Basque Government. The methodology used can serve as a reference in the development of other georoutes. A georoute brochure of the Ignatian Way across the Basque Country is presented.The maps and geological cross-sections of the Ignatian Way increase the tourist offer: spiritual, cultural, sports and gastronomic.The compiled information is freely available in institutional websites. A georoute brochure of the Ignatian Way across the Basque Country is presented. The maps and geological cross-sections of the Ignatian Way increase the tourist offer: spiritual, cultural, sports and gastronomic. The compiled information is freely available in institutional websites.
DOI: 10.15468/dl.y6jmtf
title: Occurrence Download

description: A dataset containing 100 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Curaçao, Czechia, Germany)",
 "TaxonKey is one of (, Elasmobranchii, Holocephali, Myxini)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "BasisOfRecord is one of (Human Observation, Observation, Machine Observation, Specimen, Material sample, Living Specimen)",
 "Year is 2022"
 ]
}

 The dataset includes 100 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0064049-251120083545085/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.17563570
title: "Information–Intent Resonance Framework: Phase-55 Experimental Validation (γ–δ mini series)"

description: Abstract (English)This dataset presents Phase-55 (γ–δ mini) of the Information–Intent Resonance Framework, an evolutionary extension of the Info-Gravity Theory.It introduces the coupling of informational, intentional, and observational tensors within a unified field equation.The archive includes experimental logs (.csv), metadata (.json), and documentation for reproducibility and further theoretical analysis.

概要(日本語)本データセットは「情報重力理論」の進化段階である Phase-55(γ–δ mini) に対応し、情報・意志・観測テンソルの統一構造を提示します。理論的整合性と実験データをZenodo上で公開することで、後続研究および検証を支援します。
DOI: 10.5281/zenodo.18034896
title: Anonymized survey dataset: workforce/HR software adoption in Erbil (Iraq)

description: This dataset contains anonymized survey responses collected from companies in Erbil city (Iraq) to study software adoption related to workforce management and HR information systems. The underlying study used an analytical and descriptive approach and collected responses via a questionnaire targeting organizations in both the private and public sectors in Erbil.
DOI: 10.5281/zenodo.18034897
title: Anonymized survey dataset: workforce/HR software adoption in Erbil (Iraq)

description: This dataset contains anonymized survey responses collected from companies in Erbil city (Iraq) to study software adoption related to workforce management and HR information systems. The underlying study used an analytical and descriptive approach and collected responses via a questionnaire targeting organizations in both the private and public sectors in Erbil.
DOI: 10.5281/zenodo.17545991
title: Self-Regulating Field Model (SRFM) — Safe Theory v1.0

description: SRFM (Self-Regulating Field Model) is a theoretical framework describing autonomousself-regulation in information systems through dynamic feedback mechanisms. Thissafe-release package contains a simplified version of SRFM suitable for academicreview without exposing sensitive components. It includes reproducible toy dataset,safe mathematical expressions, conceptual diagrams, scripts for figure generation,and English/Japanese PDF documents. This release is intended for researchersin AI system stability, feedback control, theoretical physics, and informationdynamics, particularly those exploring the connection between autonomous systemsand information-based field approaches such as IGT (Information Gravity Theory).
DOI: 10.5281/zenodo.17545992
title: Information-Gravity Rotation Curve and Lens Matching Dataset (Three-Galaxy Sample)

description: This dataset contains rotation curve measurements and derived lens-mass scaling analyses for three galaxies: NGC 6503, UGC 2885, and NGC 801. These data were used to examine the radial dependence of mass scaling factors when matching rotation-curve–based enclosed mass to the effective lensing mass corresponding to an Einstein radius of θ_E = 1.47 arcsec (based on SDSS J0037–0942 lens geometry: Dl=669 Mpc, Ds=1412 Mpc, Dls=922 Mpc).

The key result is that all three galaxies show a similar monotonic decrease in the scale_mass_to_match factor as radius increases, without requiring galaxy-specific tuning of dark matter halo profiles. This suggests that an additional term contributing to gravitational curvature—interpretable as an information density component—may vary systematically with radius.

Included in this release:- Observational rotation curve data (CSV)- Processed and radius-swept scale-vs-radius results (CSV)- Reproduction scripts (Python)- Figures (scale-vs-radius and rotation curve overlays)- Short technical note summarizing the procedure and findings (PDF)

This dataset is provided to support reproducibility, reanalysis, and further theoretical or observational study.
DOI: 10.25345/c5js9hn30
title: MassIVE MSV000100317 - GNPS_Investigation of bile salt hydrolase activity reveals production of conjugated secondary bile acids
title: mzXML files and raw data files for bile acid metabolomics data associated with our paper titled: Investigation of bile salt hydrolase activity reveals production of conjugated secondary bile acids.
DOI: 10.15468/dl.xk2r5p
title: Occurrence Download

description: A dataset containing 126 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Curaçao, Czechia, Germany)",
 "TaxonKey is one of (, Elasmobranchii, Holocephali, Myxini)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "BasisOfRecord is one of (Human Observation, Observation, Machine Observation, Specimen, Material sample, Living Specimen)",
 "Year is 2023"
 ]
}

 The dataset includes 126 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0064051-251120083545085/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/exvdjh
title: Colección Ornitológica FML-Tucumán

description: La COFML se inicia a finales del siglo XIX (1887) con colecciones del Dr. Miguel Lillo, quien fue colaborado por los ornitólogos italianos Luis Dinelli y Roberto Dabbene. Desde entonces fue creciendo francamente con el aporte de destacados ornitólogos a nivel mundial como el Dr. Claes Olrog. Los registros provienen de 16 países, principalmente americanos, pero también se registran países de Europa y Oceanía, siendo Argentina y particularmente su región Noroeste lo mejor representado. Los ejemplares conservados corresponden a pieles taxidermizadas para estudios científicos y en pedestal para su exhibición. Además cuenta con esqueletos, especímenes completos preservados en fluidos conservantes, tejidos para estudios moleculares y órganos internos. Se encuentran asimismo incluidos ejemplares de diferentes grupos taxonómicos que están asociados o frecuentan ambientes de humedales y palustres de la provincia de Tucumán. De estos se destacan los del orden Charadriiformes, que representan a todas las especies registradas en la provincia.
DOI: 10.5281/zenodo.18035336
title: Positronium 1S-2S dataset
DOI: 10.5281/zenodo.18035337
title: Positronium 1S-2S dataset