cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15129/9d70d515-b93e-4246-8feb-a4877b286b6d
title: Data for: "Inspection of Nuclear Assets with Limited Access using Feature Guided Waves"

description: This dataset contains simulated SAFE, FEA, and experimental data used to generate most of the figures featured within the manuscript. The SAFE data was generated by solving the equation of dynamic equilibrium using the commercial software, COMSOL. These models predicted the existence of acoustic waves in the resistance seam weld waveguide. All files are provided with no solutions saved to minimise storage requirements. The SAFE data was analysed using MATLAB through the information provided in the manuscript and was used to generate Figure 5, 6, & 7. Additional models are provided replicating the results observed in: https://doi.org/10.1016/j.ymssp.2019.02.026. The FEA data was generated via timestep models solved in the commercial software, POGO, from Imperial College London. This confirmed the findings of the SAFE model above and verified that one type of wave could be excited and readily detect defects. Like before, the data generated was analysed using MATLAB, PogoPro, and ParaVIEW. The data generated by these models was used to create Figure 8, 9, 10, 11, 12, & 13. Again, additional models are provided replicating the results observed in: https://doi.org/10.1016/j.ymssp.2019.02.026. The experimental data was acquired using the equipment described in the manuscript. These experiments showed the findings from the simulated efforts existed in reality, and explored the nuances of exciting such a wave out with a simulated noiseless environment. Specialist equipment such as a Polytec MSA-100-3D laser Doppler vibrometer was used but could be easily swapped for an equivalent. A wavemaker from Macrodesigns LTD was used to excite the transducer. This allows for sinusoidal excitation of the transducer which is uncommon. Again, this can be replaced for an equivalent. Details of the transducer, geometry and materials of the experiments are all given in the manuscript. The data generated was again analysed using MATLAB, and was used to create Figures 17, 18, 20, 21, 23 & 25.
DOI: 10.21338/ess10cfe01
title: ESS10 - data from Contact forms, edition 1.0
DOI: 10.3886/e119472
title: Data and Code for: Do doctors improve the health care of their parents? Evidence from admission lotteries

description: To assess the importance of unequal access to medical expertise and services, we estimate the causal effects of having a child who is a doctor on parents’ mortality and health care use. We use data from parents of almost 22,000 participants in admission lotteries to medical school in the Netherlands. Our findings indicate that informal access to medical expertise and services is not an impor- tant cause of differences in health care use and mortality.
DOI: 10.3886/e119472v2
title: Data and Code for: Do doctors improve the health care of their parents? Evidence from admission lotteries

description: To assess the importance of unequal access to medical expertise and services, we estimate the causal effects of having a child who is a doctor on parents’ mortality and health care use. We use data from parents of almost 22,000 participants in admission lotteries to medical school in the Netherlands. Our findings indicate that informal access to medical expertise and services is not an impor- tant cause of differences in health care use and mortality.
DOI: 10.34740/kaggle/dsv/3851458
title: 2021 World Population (updated daily)
DOI: 10.6084/m9.figshare.20069972
title: Data for "Spontaneous brain activity abnormalities in migraine: A meta-analysis of functional neuroimaging"

description: Neuroimaging studies have demonstrated that migraine is accompanied by spontaneous brain activity alterations in specific regions. However, these findings are inconsistent, thus hindering our understanding of the potential neuropathology. Hence, we performed a quantitative whole-brain meta-analysis of relevant resting-state functional imaging studies to identify brain regions consistently involved in migraine. <br> A systematic search of studies that investigated the differences in spontaneous brain activity patterns between migraineurs and healthy controls (HCs) up to April 2022 was conducted. We then performed a whole-brain voxel-wise meta-analysis using the anisotropic effect size version of seed-based <em>d</em> mapping software. Complementary analyses including jackknife sensitivity analysis, heterogeneity test, publication bias test, subgroup analysis and meta-regression analysis were conducted as well. <br> In total, 24 studies that reported 31 datasets were finally eligible for our meta-analysis, including 748 patients with migraine and 690 HCs. In contrast to HCs, migraineurs demonstrated consistent and robust decreased spontaneous brain activity in the angular gyrus, visual cortex and cerebellum, and increased activity in the caudate, thalamus, pons and prefrontal cortex. Results were robust and highly replicable in the following jackknife sensitivity analysis and subgroup analysis. Meta-regression analyses revealed that a higher visual analogue scale score in the patient sample was associated with increased spontaneous brain activity in the left thalamus. <br> These findings provided not only a comprehensive overview of spontaneous brain activity patterns impairments, but also useful insights into the pathophysiology of dysfunction in migraine.
DOI: 10.6084/m9.figshare.20069972.v2
title: Data for "Spontaneous brain activity abnormalities in migraine: A meta-analysis of functional neuroimaging"

description: Neuroimaging studies have demonstrated that migraine is accompanied by spontaneous brain activity alterations in specific regions. However, these findings are inconsistent, thus hindering our understanding of the potential neuropathology. Hence, we performed a quantitative whole-brain meta-analysis of relevant resting-state functional imaging studies to identify brain regions consistently involved in migraine. <br> A systematic search of studies that investigated the differences in spontaneous brain activity patterns between migraineurs and healthy controls (HCs) up to April 2022 was conducted. We then performed a whole-brain voxel-wise meta-analysis using the anisotropic effect size version of seed-based <em>d</em> mapping software. Complementary analyses including jackknife sensitivity analysis, heterogeneity test, publication bias test, subgroup analysis and meta-regression analysis were conducted as well. <br> In total, 24 studies that reported 31 datasets were finally eligible for our meta-analysis, including 748 patients with migraine and 690 HCs. In contrast to HCs, migraineurs demonstrated consistent and robust decreased spontaneous brain activity in the angular gyrus, visual cortex and cerebellum, and increased activity in the caudate, thalamus, pons and prefrontal cortex. Results were robust and highly replicable in the following jackknife sensitivity analysis and subgroup analysis. Meta-regression analyses revealed that a higher visual analogue scale score in the patient sample was associated with increased spontaneous brain activity in the left thalamus. <br> These findings provided not only a comprehensive overview of spontaneous brain activity patterns impairments, but also useful insights into the pathophysiology of dysfunction in migraine.
DOI: 10.6084/m9.figshare.20069972.v1
title: Data for "Spontaneous brain activity abnormalities in migraine: A meta-analysis of resting-state functional imaging"

description: Neuroimaging studies have demonstrated that migraine is accompanied by spontaneous brain activity alterations in specific regions. However, these findings are inconsistent, thus hindering our understanding of the potential neuropathology. Hence, we performed a quantitative whole-brain meta-analysis of relevant resting-state functional imaging studies to identify brain regions consistently involved in migraine. <br> A systematic search of studies that investigated the differences in spontaneous brain activity patterns between migraineurs and healthy controls (HCs) up to April 2022 was conducted. We then performed a whole-brain voxel-wise meta-analysis using the anisotropic effect size version of seed-based <em>d</em> mapping software. Complementary analyses including jackknife sensitivity analysis, heterogeneity test, publication bias test, subgroup analysis and meta-regression analysis were conducted as well. <br> In total, 24 studies that reported 31 datasets were finally eligible for our meta-analysis, including 748 patients with migraine and 690 HCs. In contrast to HCs, migraineurs demonstrated consistent and robust decreased spontaneous brain activity in the angular gyrus, visual cortex and cerebellum, and increased activity in the caudate, thalamus, pons and prefrontal cortex. Results were robust and highly replicable in the following jackknife sensitivity analysis and subgroup analysis. Meta-regression analyses revealed that a higher visual analogue scale score in the patient sample was associated with increased spontaneous brain activity in the left thalamus. <br> These findings provided not only a comprehensive overview of spontaneous brain activity patterns impairments, but also useful insights into the pathophysiology of dysfunction in migraine.
DOI: 10.5525/gla.researchdata.1120
title: Clinical psychologists' views of telephone-based therapies for children and adolescents during COVID-19 in Scotland

description: This dataset includes transcripts conducted with child and adolescent clinical psychologists based in the UK and their views on delivering telephone therapies during the COVID-19 pandemic.
DOI: 10.7303/syn32167669
title: Pólis PCDaS
DOI: 10.6084/m9.figshare.15161153
title: The Colombian geochronological database (CGD)

description: Geochronological databases are powerful tools for characterizing the crustal evolution and the age spectra of a region and allow comparison with other areas at a regional scale. In this contribution, we present the Colombian Geochronological Database (CGD), which contains a curated compilation of ca. 67,406 individual published U-Th-Pb, K-Ar, Ar-Ar, Rb-Sr, Sm-Nd, Lu-Hf, Fission-track, U-Th-He, and Re-Os mineral and whole rock ages that are reported in the published literature. Each date includes geographic coordinates, geological setting, petrologic and chemical information extracted from the respective publications. The structure of the database provides a powerful interface for constructing queries and allows searching and extracting information on geographic domains, provinces, stratigraphic units, isotopic systems, date interpretations, references, etc. This information establishes a framework for regional and global geological interpretations with geochronological, stratigraphic, structural and palaeogeographic implications. With the present effort we present to the geoscience community a clear insight, from a regional perspective, to the geology and tectonics of Colombia since Precambrian times. The comparison of all (detrital and magmatic) single zircon U-Pb dates from the Colombian (Gondwana sourced) geochronological database with the Global and North American (Laurentia sourced) databases provides a temporal constraint on the evolution of the South American continent. U-Pb zircon ages in Colombia define 13 peak clusters centred at 1767, 1530, 1325, 1178, 1007, 605,540, 468, 271, 237, 182, 76 and 10 Ma but of those, only few have a good correlation in all three databases: 1007 (Grenvillian/Orinoquian/Putumayo Orogeny), 605 (Braziliano/Pan-African Orogeny), 468 (Famatinian/Taconic Orogeny), and 182 Ma (Break-up of Pangea) zircon peaks. This correlation suggests that some tectonic events in Colombia are global and might represent crustal production and preservation while the other peaks might just represent local arc magmatic events.
DOI: 10.6084/m9.figshare.16418850.v1
title: Sedimentological and geochemical characteristics of Lower Jurassic Sandstones from Gümüşhane, NE Turkey: implications for source to sink processes, paleoenvironmental conditions, provenance and tectonic settings

description: The eastern Sakarya Zone (SZ), one of the Alpine Himalayan Belt’s main components, has complex Mesozoic–Cenozoic geodynamic evolution, which remains controversial. Early-Middle Jurassic volcano-sedimentary successions (Şenköy Formation) extensively outcrops in Gümüşhane region, NE Turkey. It is regarded as a critical unit to understand the Mesozoic tectonic evolution of the eastern Sakarya Zone. One of the Şenköy Formation’s predominant units is sandstone succession, preserving implications for paleoenvironmental conditions and tectono-sedimentary development of Neotethys Ocean. Thus, a combined analysis of comprehensive petrography, whole-rock major, trace and rare earth element data is carried out on the sandstones, which are well constrained as late Sinemurian- Pliensbachian. The sandstones are mainly arkosic to lithic arenites in lithology showing poor textural maturities. They are mostly represented by relatively high ICV, low CIA, high K<sub>2</sub>O/Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>+ MgO, TiO<sub>2</sub>, Th/U, pronounced negative Eu anomaly, enriched LREEs, elevated Gd<sub>N</sub>/Yb<sub>N</sub>, low Ce/Ce*, Ni/Co, La/V and Zr/Ti. The petrographic and geochemical characteristics imply that the sediments may have experienced relatively low chemical weathering processes and slight reworking and recycling processes with a short transport distance before deposition in the basin. Early Jurassic sandstone successions were interpreted as a transgressive series, showing a predominantly open sea environment with oxidizing paleoenvironmental conditions. The sandstone samples’ paleoenvironment is likely to be located along the southern margin of the arc and the Neotethyan basin to the south. The extensional and trans-extensional tectonic regime might have played an essential role in controlling the basin’s isolated-half graben and/or asymmetric geometry, leading to changes in the provenance of studied sandstone samples. Thus, the geochemical signature differences are probably associated with basement-related proximal origins and minor effects of the multi-phases petrogenesis that experienced different source to sink processes. Early Jurassic sandstones were probably derived from multi-genetic source rocks, including (i) granite and (ii) metamorphic rocks. Our new data has also indicated that other source rocks can include mafic to felsic volcanic succession. The possible provenance for granitic pluton and metamorphic rocks can be provided by the Hercynian heterogenetic crystalline basement widespread throughout the SZ. However, mafic to felsic volcanic rock source is likely to be associated with the pre-Early Jurassic nearby volcanic-arc, which is rarely recorded in the eastern SZ. The source rock signatures may imply a close genetic link with ancient magmatic-arc generation due to the southward subduction of Palaeotethys.
DOI: 10.6084/m9.figshare.15075188
title: The timing of rifting events in the easternmost Mediterranean: U-Pb dating of zircons from volcanic rocks in the Levant margin

description: The Levant basin, at the easternmost Mediterranean, formed during the opening of the Neo-Tethys at Permian to Jurassic times, as recorded by subsidence and magmatism along its SE passive margin. While the subsurface extensional structure was reconstructed in detail, the spatial and temporal distribution of igneous activity is not well known. Here we present new SIMS U-Pb dating of zircons from rifting related volcanic sequences recovered from four deep boreholes in the Levant margin of coastal Israel. The Asher volcanics, a deeply buried 2.5 km thick basaltic sequence, which accumulated within fault-bounded basin, was previously dated by K-Ar and Ar-Ar to early Jurassic times. Zircons (n=46) separated from the bottom and top of the volcanic sequence yielded 206±2 Ma and 205 to 202 Ma, respectively, indicating that Asher volcanics are of Late Triassic (Rhaetian) age. Zircon xenocrysts indicate Permian (289±2 Ma) felsic magmatism. Rifting activity in the Levant margin included several Permian-Triassic pulses of faulting and subsidence, with a prolonged magmatism-bearing rifting event at Late Carnian to Rhaetian times (~230-201 Ma). Pulsed rifting is also indicated in the conjugate, northern, margin of the southern Neo-Tethys, and the timing of subsidence and magmatic pulses well correlate to the Levant margin.
DOI: 10.6084/m9.figshare.15075188.v3
title: The timing of rifting events in the easternmost Mediterranean: U-Pb dating of zircons from volcanic rocks in the Levant margin

description: The Levant basin, at the easternmost Mediterranean, formed during the opening of the Neo-Tethys at Permian to Jurassic times, as recorded by subsidence and magmatism along its SE passive margin. While the subsurface extensional structure was reconstructed in detail, the spatial and temporal distribution of igneous activity is not well known. Here we present new SIMS U-Pb dating of zircons from rifting related volcanic sequences recovered from four deep boreholes in the Levant margin of coastal Israel. The Asher volcanics, a deeply buried 2.5 km thick basaltic sequence, which accumulated within fault-bounded basin, was previously dated by K-Ar and Ar-Ar to early Jurassic times. Zircons (n=46) separated from the bottom and top of the volcanic sequence yielded 206±2 Ma and 205 to 202 Ma, respectively, indicating that Asher volcanics are of Late Triassic (Rhaetian) age. Zircon xenocrysts indicate Permian (289±2 Ma) felsic magmatism. Rifting activity in the Levant margin included several Permian-Triassic pulses of faulting and subsidence, with a prolonged magmatism-bearing rifting event at Late Carnian to Rhaetian times (~230-201 Ma). Pulsed rifting is also indicated in the conjugate, northern, margin of the southern Neo-Tethys, and the timing of subsidence and magmatic pulses well correlate to the Levant margin.
DOI: 10.6084/m9.figshare.15161153.v3
title: The Colombian geochronological database (CGD)

description: Geochronological databases are powerful tools for characterizing the crustal evolution and the age spectra of a region and allow comparison with other areas at a regional scale. In this contribution, we present the Colombian Geochronological Database (CGD), which contains a curated compilation of ca. 67,406 individual published U-Th-Pb, K-Ar, Ar-Ar, Rb-Sr, Sm-Nd, Lu-Hf, Fission-track, U-Th-He, and Re-Os mineral and whole rock ages that are reported in the published literature. Each date includes geographic coordinates, geological setting, petrologic and chemical information extracted from the respective publications. The structure of the database provides a powerful interface for constructing queries and allows searching and extracting information on geographic domains, provinces, stratigraphic units, isotopic systems, date interpretations, references, etc. This information establishes a framework for regional and global geological interpretations with geochronological, stratigraphic, structural and palaeogeographic implications. With the present effort we present to the geoscience community a clear insight, from a regional perspective, to the geology and tectonics of Colombia since Precambrian times. The comparison of all (detrital and magmatic) single zircon U-Pb dates from the Colombian (Gondwana sourced) geochronological database with the Global and North American (Laurentia sourced) databases provides a temporal constraint on the evolution of the South American continent. U-Pb zircon ages in Colombia define 13 peak clusters centred at 1767, 1530, 1325, 1178, 1007, 605,540, 468, 271, 237, 182, 76 and 10 Ma but of those, only few have a good correlation in all three databases: 1007 (Grenvillian/Orinoquian/Putumayo Orogeny), 605 (Braziliano/Pan-African Orogeny), 468 (Famatinian/Taconic Orogeny), and 182 Ma (Break-up of Pangea) zircon peaks. This correlation suggests that some tectonic events in Colombia are global and might represent crustal production and preservation while the other peaks might just represent local arc magmatic events.
DOI: 10.6084/m9.figshare.16418850
title: Sedimentological and geochemical characteristics of Lower Jurassic Sandstones from Gümüşhane, NE Turkey: implications for source to sink processes, paleoenvironmental conditions, provenance and tectonic settings

description: The eastern Sakarya Zone (SZ), one of the Alpine Himalayan Belt’s main components, has complex Mesozoic–Cenozoic geodynamic evolution, which remains controversial. Early-Middle Jurassic volcano-sedimentary successions (Şenköy Formation) extensively outcrops in Gümüşhane region, NE Turkey. It is regarded as a critical unit to understand the Mesozoic tectonic evolution of the eastern Sakarya Zone. One of the Şenköy Formation’s predominant units is sandstone succession, preserving implications for paleoenvironmental conditions and tectono-sedimentary development of Neotethys Ocean. Thus, a combined analysis of comprehensive petrography, whole-rock major, trace and rare earth element data is carried out on the sandstones, which are well constrained as late Sinemurian- Pliensbachian. The sandstones are mainly arkosic to lithic arenites in lithology showing poor textural maturities. They are mostly represented by relatively high ICV, low CIA, high K<sub>2</sub>O/Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>+ MgO, TiO<sub>2</sub>, Th/U, pronounced negative Eu anomaly, enriched LREEs, elevated Gd<sub>N</sub>/Yb<sub>N</sub>, low Ce/Ce*, Ni/Co, La/V and Zr/Ti. The petrographic and geochemical characteristics imply that the sediments may have experienced relatively low chemical weathering processes and slight reworking and recycling processes with a short transport distance before deposition in the basin. Early Jurassic sandstone successions were interpreted as a transgressive series, showing a predominantly open sea environment with oxidizing paleoenvironmental conditions. The sandstone samples’ paleoenvironment is likely to be located along the southern margin of the arc and the Neotethyan basin to the south. The extensional and trans-extensional tectonic regime might have played an essential role in controlling the basin’s isolated-half graben and/or asymmetric geometry, leading to changes in the provenance of studied sandstone samples. Thus, the geochemical signature differences are probably associated with basement-related proximal origins and minor effects of the multi-phases petrogenesis that experienced different source to sink processes. Early Jurassic sandstones were probably derived from multi-genetic source rocks, including (i) granite and (ii) metamorphic rocks. Our new data has also indicated that other source rocks can include mafic to felsic volcanic succession. The possible provenance for granitic pluton and metamorphic rocks can be provided by the Hercynian heterogenetic crystalline basement widespread throughout the SZ. However, mafic to felsic volcanic rock source is likely to be associated with the pre-Early Jurassic nearby volcanic-arc, which is rarely recorded in the eastern SZ. The source rock signatures may imply a close genetic link with ancient magmatic-arc generation due to the southward subduction of Palaeotethys.