cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.24550807
title: History of western Tethys Ocean and the birth of the circum-mediterranean orogeny as reflected by source-to-sink relations

description: A broad region of Mesozoic to Cenozoic tectonism along the western and central Circum-Mediterranean (CM) margins, from southern Spain (Betic Cordillera) to the northern Morocco (Rif) and Italy (Apennines), includes huge volumes of sedimentary record since the Late Paleozoic. These sediments are contemporaneous and related with the fragmentation of the Pangean supercontinent due to the rifting and progressive closure, as well as the following birth of the CM orogeny. The composition and stratigraphic relations of clastics in diverse sedimentary basins of the CM region reflect a complete record of provenance relations related to the progressive destruction of the Neotethyan Ocean and plate convergence between the two major plates of Europe and Africa, and Iberia, Adria and Mesomediterranean micrplates located between them. The changing nature of clastic wedges reflects the provenance relations from different source rocks involving obduction of the oceanic lithosphere, the uplifted Alpine-Mediterranean Chains, and the accreted previously deformed Mesomediterranean Microplate (AlKaPeCa), as well local neovolcanic sources, within the spatial and temporal evolving geo-puzzle terranes of the CM orogeny. The provenance evolution of sediment provides insights into how plate convergence and continental collision direct the sediment dispersal pathway in Cenozoic basins due to closure of eastern and southern Alpine-Tethyan remnant ocean basins and to the dual dispersal pathways from the previously born Alps and the nascent AlKaPeCa at the expenses of the previously deformed Mesomediterranean terranes. The source-to-sink relations testify episodic deformation events, diachronous Tethyan basin development, differentiate sediment provenance from exhumed and uplifted Alpine and CM orogens, and palaeogeographic rearrangement of crustal blocks along the nascent Mediterranean region.
DOI: 10.6084/m9.figshare.24550807.v1
title: History of western Tethys Ocean and the birth of the circum-mediterranean orogeny as reflected by source-to-sink relations

description: A broad region of Mesozoic to Cenozoic tectonism along the western and central Circum-Mediterranean (CM) margins, from southern Spain (Betic Cordillera) to the northern Morocco (Rif) and Italy (Apennines), includes huge volumes of sedimentary record since the Late Paleozoic. These sediments are contemporaneous and related with the fragmentation of the Pangean supercontinent due to the rifting and progressive closure, as well as the following birth of the CM orogeny. The composition and stratigraphic relations of clastics in diverse sedimentary basins of the CM region reflect a complete record of provenance relations related to the progressive destruction of the Neotethyan Ocean and plate convergence between the two major plates of Europe and Africa, and Iberia, Adria and Mesomediterranean micrplates located between them. The changing nature of clastic wedges reflects the provenance relations from different source rocks involving obduction of the oceanic lithosphere, the uplifted Alpine-Mediterranean Chains, and the accreted previously deformed Mesomediterranean Microplate (AlKaPeCa), as well local neovolcanic sources, within the spatial and temporal evolving geo-puzzle terranes of the CM orogeny. The provenance evolution of sediment provides insights into how plate convergence and continental collision direct the sediment dispersal pathway in Cenozoic basins due to closure of eastern and southern Alpine-Tethyan remnant ocean basins and to the dual dispersal pathways from the previously born Alps and the nascent AlKaPeCa at the expenses of the previously deformed Mesomediterranean terranes. The source-to-sink relations testify episodic deformation events, diachronous Tethyan basin development, differentiate sediment provenance from exhumed and uplifted Alpine and CM orogens, and palaeogeographic rearrangement of crustal blocks along the nascent Mediterranean region.
DOI: 10.6084/m9.figshare.22638874
title: Petrogenesis of Late Campanian Alkaline Igneous Rocks in Eastern Anatolia: Magmatism related to a subduction transform edge propagator (STEP) fault?

description: In eastern Anatolia, the Divriği-Hekimhan Magmatic Province (DHMP) includes ~77–69 Ma alkaline rock units which are located to the NW of the Baskil Arc of ~85–74 Ma. The magmatic rocks are composed of nepheline (Ne)–to quartz (Q)–normative alkaline basaltic to trachytic/syenitic units. Among them, the basaltic rocks are composed of plagioclase (Or<sub>2–11</sub>Ab<sub>32–51</sub>An<sub>39–64</sub>) + clinopyroxene (Wo<sub>47–51</sub>En<sub>35–42</sub>Fs<sub>9–16</sub>) + Fe-Ti oxide ± alkali feldspar (Or<sub>57–98</sub>Ab<sub>2–42</sub>An<sub>1</sub>) ± biotite ± olivine. Their <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(<i>I</i>)</sub> ratios and ɛNd<sub>(<i>I</i>)</sub> values vary in the ranges of 0.70591–0.70871 and−3.2–1.6, respectively. The subvolcanic trachytic rocks are composed of perthitic alkali feldspar phenocryst in a matrix of feldspar (Or<sub>45–61</sub>Ab<sub>38–54</sub>An<sub>0–2</sub>), biotite, and Fe-Ti oxides. The trachytic volcanic rocks are made up of feldspar (Or<sub>38–63</sub>Ab<sub>34–59</sub>An<sub>1–4</sub>) in a fine-grained matrix. Their <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(<i>I</i>)</sub> ratios and ɛNd<sub>(<i>I</i>)</sub> values vary in the ranges of 0.70532–0.70952 and−3.2–0.7, respectively. The syenitic rocks in the region contain both quartz- and nepheline-sodalite-bearing syenites. Geochemical features reveal that the Ne-normative basaltic magmas have undergone mafic mineral fractionation coupled with crustal contamination to produce the Q-normative derivatives. Enhanced differentiation of the Ne- and Q-normative fractionated magmas via feldspar-dominated fractionation created the silica-undersaturated and -oversaturated trachytic magmas, respectively. During the feldspar-dominated differentiation, the re-melting of accumulated alkali feldspars in the magma chamber likely gave rise to the formation of trachytic rocks with alkali feldspar-like whole rock compositions. The final products of the Ne-normative magmas are represented by the phonolites and foid-syenites with silica-undersaturated eutectic compositions. A geochemical evaluation of the basaltic rocks revealed that the alkaline magmatism mainly originated from a shallow asthenospheric mantle source which had previously been metasomatized by oceanic to continental subduction. We suggest that the DHMP was formed in response to STEP fault-controlled rolling back of the northward subducting slab of the Baskil Arc, which created a localized gap for asthenospheric upwelling.
DOI: 10.6084/m9.figshare.22638874.v1
title: Petrogenesis of Late Campanian Alkaline Igneous Rocks in Eastern Anatolia: Magmatism related to a subduction transform edge propagator (STEP) fault?

description: In eastern Anatolia, the Divriği-Hekimhan Magmatic Province (DHMP) includes ~77–69 Ma alkaline rock units which are located to the NW of the Baskil Arc of ~85–74 Ma. The magmatic rocks are composed of nepheline (Ne)–to quartz (Q)–normative alkaline basaltic to trachytic/syenitic units. Among them, the basaltic rocks are composed of plagioclase (Or<sub>2–11</sub>Ab<sub>32–51</sub>An<sub>39–64</sub>) + clinopyroxene (Wo<sub>47–51</sub>En<sub>35–42</sub>Fs<sub>9–16</sub>) + Fe-Ti oxide ± alkali feldspar (Or<sub>57–98</sub>Ab<sub>2–42</sub>An<sub>1</sub>) ± biotite ± olivine. Their <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(<i>I</i>)</sub> ratios and ɛNd<sub>(<i>I</i>)</sub> values vary in the ranges of 0.70591–0.70871 and−3.2–1.6, respectively. The subvolcanic trachytic rocks are composed of perthitic alkali feldspar phenocryst in a matrix of feldspar (Or<sub>45–61</sub>Ab<sub>38–54</sub>An<sub>0–2</sub>), biotite, and Fe-Ti oxides. The trachytic volcanic rocks are made up of feldspar (Or<sub>38–63</sub>Ab<sub>34–59</sub>An<sub>1–4</sub>) in a fine-grained matrix. Their <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(<i>I</i>)</sub> ratios and ɛNd<sub>(<i>I</i>)</sub> values vary in the ranges of 0.70532–0.70952 and−3.2–0.7, respectively. The syenitic rocks in the region contain both quartz- and nepheline-sodalite-bearing syenites. Geochemical features reveal that the Ne-normative basaltic magmas have undergone mafic mineral fractionation coupled with crustal contamination to produce the Q-normative derivatives. Enhanced differentiation of the Ne- and Q-normative fractionated magmas via feldspar-dominated fractionation created the silica-undersaturated and -oversaturated trachytic magmas, respectively. During the feldspar-dominated differentiation, the re-melting of accumulated alkali feldspars in the magma chamber likely gave rise to the formation of trachytic rocks with alkali feldspar-like whole rock compositions. The final products of the Ne-normative magmas are represented by the phonolites and foid-syenites with silica-undersaturated eutectic compositions. A geochemical evaluation of the basaltic rocks revealed that the alkaline magmatism mainly originated from a shallow asthenospheric mantle source which had previously been metasomatized by oceanic to continental subduction. We suggest that the DHMP was formed in response to STEP fault-controlled rolling back of the northward subducting slab of the Baskil Arc, which created a localized gap for asthenospheric upwelling.
DOI: 10.6084/m9.figshare.22791243
title: Alpine convergence record in the Carboniferous Badstub Formation, Upper Austroalpine basement nappes, Austria

description: Within the Carboniferous of Nötsch, the Badstub Formation is a clastic sequence of the Upper Austroalpine basement nappes exposed few kilometres north of the Periadriatic Fault System (Carinthia, Austria). Although these rocks preserve pristine sedimentary features, multi-scale structural analysis disclosed a syn-metamorphic foliation in fine-grained rocks, sets of mineralized faults, veins, and corona textures. Vein fillings and coronas contain equilibrium mineral assemblages with prehnite, pumpellyite, chlorite, phengitic mica, winchite, and riebeckite. Thermodynamic modelling and geothermometry constrain metamorphic conditions at 260–310°C and 0.25–0.50 GPa that are consistent with a temperature/depth ratio of about 20°C km<sup>−1</sup>. In a 2D thermomechanical model this thermal state is reached either in the upper or lower continental plate during convergence. Thus, during the Alpine convergence, the Badstub rocks were buried from the shallow crust at depths between 13 and 18 km either by ablative oceanic subduction or by continental subduction of the passive margin, and eventually stacked into the orogenic wedge at the Adria margin. During the downward and upward paths, the Badstub rocks were translated as a coherent poorly strained block. This first quantitative constraint on metamorphism for these Carboniferous rocks is consistent with the Upper Austroalpine basement nappes being a tectonic system that recorded the Alpine convergence under eclogite to prehnite–pumpellyite facies conditions.
DOI: 10.6084/m9.figshare.22800405.v1
title: Evolution of Aptian and Albian magmatism of Western and Northern Chukotka (Northeast Russia) based on zircon U-Pb geochronology and rock geochemistry

description: Across western and northern Chukotka, a region spanning 400 000 km<sup>2</sup>, we have defined three different tectono-magmatic systems that were active during the Aptian-Albian (123–100 Ma) time span: (1) the Tytylveem post-collisional belt (123–105 Ma); (2) the Chaun province of extension-related magmatism (109–100 Ma); and (3) the earliest eruptive units (106–100 Ma) of the subduction-related Okhotsk-Chukotka volcanic belt (OCVB). The observed tectono-magmatic systems are characterized by their location and by their different chemical and isotopic compositions. The general enrichment of magma sources successively increases from the OCVB to the Tytylveem belt and then to the Chaun province. While the Tytylveem belt was active, the volcanic loci shifted northwest along the strike of the belt, perhaps because of diachronous delamination of the lithosphere of the once present, but extinct, South Anyui ocean. On the scale of the entire region of NE Asia, the tectonic re-arrangement that controlled magmatism in the Early Cretaceous was marked by the extinction of major subduction zones on the periphery of the closing Oimyakon and South Anyui oceanic basins followed by magmatic events likely caused by lithospheric delamination and/or extension. Along the Pacific margin of Asia, subduction-related volcanism was nearly continuous during the entire Cretaceous.
DOI: 10.17632/pk3wv93s3m.1
title: Issues, comments and projects from four popular Issue Tracking Systems

description: Data of issues, comments and projects from four popular Issue Tracking Systems.
DOI: 10.6084/m9.figshare.22574524.v1
title: New palaeoclimatic constraints from paleosols on the Middle-Late Jurassic landscape, Western Colorado, U.S.A

description: The Wanakah Formation and Tidwell Member of the Morrison Formation record intervals of paedogenesis in the Paradox Basin and Central Colorado trough, western Colorado during the Middle-Late Jurassic. Detailed field description of paleosols and paedogenic carbonates at different stratigraphic horizons from three localities document four main pedotypes: vertisols, gleysols, oxisols, and protosols. Generally, gleysols reflect reducing conditions, protosols and oxisols reflect oxidizing conditions, and vertisols reflect fluctuations in oxidizing/reducing conditions (seasonality). Major elemental geochemical ratios in samples from these paleosols suggest variable redox conditions and a sub-humid to humid paleoclimate with seasonal precipitations during paleosol development. Estimated mean annual temperature based on elemental analyses of paleosol B in paleosols from Ribbon Trail and Escalante Canyon in western Colorado suggest mesic – thermic paleoclimate. Mean annual precipitation indicates sub-humid to humid regional palaeoclimatic conditions marked by seasonal precipitation. Clay mineralogy of these paleosols, determined by X-ray diffraction, shows the abundance of illite most likely formed from smectite alteration due to episodic wetting and drying. δ<sup>13</sup>C and δ<sup>18</sup>O isotope analyses of carbonate veins in these paleosols suggest that they formed recently from meteoric water and therefore are not considered for palaeoclimatic reconstructions. Mean annual temperature and mean annual precipitation estimates in the Wanakah Formation and Tidwell Member of the Morrison Formation provide new information on the local and regional palaeoclimatic and paleoenvironmental conditions during the Middle Jurassic in western Colorado as well as data for comparison with the Upper Morrison paleoclimate from northern and southern localities in the western United States.
DOI: 10.17632/pk3wv93s3m.2
title: Issues, comments and projects from four popular Issue Tracking Systems

description: Data of issues, comments and projects from four popular Issue Tracking Systems.
DOI: 10.6084/m9.figshare.22574524
title: New palaeoclimatic constraints from paleosols on the Middle-Late Jurassic landscape, Western Colorado, U.S.A

description: The Wanakah Formation and Tidwell Member of the Morrison Formation record intervals of paedogenesis in the Paradox Basin and Central Colorado trough, western Colorado during the Middle-Late Jurassic. Detailed field description of paleosols and paedogenic carbonates at different stratigraphic horizons from three localities document four main pedotypes: vertisols, gleysols, oxisols, and protosols. Generally, gleysols reflect reducing conditions, protosols and oxisols reflect oxidizing conditions, and vertisols reflect fluctuations in oxidizing/reducing conditions (seasonality). Major elemental geochemical ratios in samples from these paleosols suggest variable redox conditions and a sub-humid to humid paleoclimate with seasonal precipitations during paleosol development. Estimated mean annual temperature based on elemental analyses of paleosol B in paleosols from Ribbon Trail and Escalante Canyon in western Colorado suggest mesic – thermic paleoclimate. Mean annual precipitation indicates sub-humid to humid regional palaeoclimatic conditions marked by seasonal precipitation. Clay mineralogy of these paleosols, determined by X-ray diffraction, shows the abundance of illite most likely formed from smectite alteration due to episodic wetting and drying. δ<sup>13</sup>C and δ<sup>18</sup>O isotope analyses of carbonate veins in these paleosols suggest that they formed recently from meteoric water and therefore are not considered for palaeoclimatic reconstructions. Mean annual temperature and mean annual precipitation estimates in the Wanakah Formation and Tidwell Member of the Morrison Formation provide new information on the local and regional palaeoclimatic and paleoenvironmental conditions during the Middle Jurassic in western Colorado as well as data for comparison with the Upper Morrison paleoclimate from northern and southern localities in the western United States.
DOI: 10.6084/m9.figshare.22791243.v1
title: Alpine convergence record in the Carboniferous Badstub Formation, Upper Austroalpine basement nappes, Austria

description: Within the Carboniferous of Nötsch, the Badstub Formation is a clastic sequence of the Upper Austroalpine basement nappes exposed few kilometres north of the Periadriatic Fault System (Carinthia, Austria). Although these rocks preserve pristine sedimentary features, multi-scale structural analysis disclosed a syn-metamorphic foliation in fine-grained rocks, sets of mineralized faults, veins, and corona textures. Vein fillings and coronas contain equilibrium mineral assemblages with prehnite, pumpellyite, chlorite, phengitic mica, winchite, and riebeckite. Thermodynamic modelling and geothermometry constrain metamorphic conditions at 260–310°C and 0.25–0.50 GPa that are consistent with a temperature/depth ratio of about 20°C km<sup>−1</sup>. In a 2D thermomechanical model this thermal state is reached either in the upper or lower continental plate during convergence. Thus, during the Alpine convergence, the Badstub rocks were buried from the shallow crust at depths between 13 and 18 km either by ablative oceanic subduction or by continental subduction of the passive margin, and eventually stacked into the orogenic wedge at the Adria margin. During the downward and upward paths, the Badstub rocks were translated as a coherent poorly strained block. This first quantitative constraint on metamorphism for these Carboniferous rocks is consistent with the Upper Austroalpine basement nappes being a tectonic system that recorded the Alpine convergence under eclogite to prehnite–pumpellyite facies conditions.
DOI: 10.17632/62jsjt2pb6.1
title: Assessing the Latest Advances in Bone Marrow Stem Cell Therapy for Avascular Necrosis Hip: A Comprehensive Systematic Review and Meta-Analysis

description: This is the Prisma Checklist of Assessing the Latest Advances in Bone Marrow Stem Cell Therapy for Avascular Necrosis Hip: A Comprehensive Systematic Review and Meta-Analysis
DOI: 10.17632/5bshhfg2js.1
title: Data Set- The Effect of Co-Branding and Brand Prestige on Perceived Quality and Purchase Decisions

description: This study examines the influence of co-branding and brand prestige on perceived quality and their impact on purchase decisions. This study contributes to the marketing literature by using the co-branding and brand prestige variable to see its effect on perceived quality and purchase decisions in the beverage industry context. The study contributes to the knowledge of managerial practice by highlighting the importance of co-branding strategy and brand prestige, which shapes the consumer's perceived quality, and illustrating its impact on consumer purchase decisions. This study provides insights into a brand alliance that the right co-branding strategy and brand prestige can create a consumer purchase decision.
DOI: 10.17632/7xx4bc292f.2
title: Data in Brief - Urban hot spots - Amazon - Brazil

description: The file contains a workbook in .xlxs format with two spreadsheets, the first with the filtered data at each of the 22 collection points separated by date and time, temperature and relative humidity. The second spreadsheet contains all the raw data collected throughout the research period. This data was collected on November 5, 2023, using a U23-001 outdoor temperature and humidity data logger. The device was programmed to record data every minute, and all observations were made on a single day. The device has software called HOBOware, which allows data to be downloaded via a USB port. In total, 88 records were obtained at 9am, 12pm, 3pm and 6pm at 22 points in the historic center of Santarém-PA. The total area covered was approximately 27.6 hectares with a perimeter of over 2 km. A car was used to travel between the points, although in some situations it was necessary to walk.
DOI: 10.17632/7xx4bc292f.1
title: Data in Brief - Dezember 2023

description: The file contains a workbook in .xlxs format with two spreadsheets, the first with the filtered data at each of the 22 collection points separated by date and time, temperature and relative humidity. The second spreadsheet contains all the raw data collected throughout the research period. This data was collected on November 5, 2023, using a U23-001 outdoor temperature and humidity data logger. The device was programmed to record data every minute, and all observations were made on a single day. The device has software called HOBOware, which allows data to be downloaded via a USB port. In total, 88 records were obtained at 9am, 12pm, 3pm and 6pm at 22 points in the historic center of Santarém-PA. The total area covered was approximately 27.6 hectares with a perimeter of over 2 km. A car was used to travel between the points, although in some situations it was necessary to walk.
DOI: 10.17632/7xx4bc292f.3
title: Data in Brief - Urban hot spots - Amazon - Brazil

description: The file contains a workbook in .xlxs format with two spreadsheets, the first with the filtered data at each of the 22 collection points separated by date and time, temperature and relative humidity. The second spreadsheet contains all the raw data collected throughout the research period. 
This data was collected on November 5, 2023, using a U23-001 outdoor temperature and humidity data logger. The device was programmed to record data every minute, and all observations were made on a single day. The device has software called HOBOware, which allows data to be downloaded via a USB port.
In total, 88 records were obtained at 9am, 12pm, 3pm and 6pm at 22 points in the historic center of Santarém-PA. The total area covered was approximately 27.6 hectares with a perimeter of over 2 km. A car was used to travel between the points, although in some situations it was necessary to walk.
DOI: 10.17632/kfx4pkbn36.1
title: State-level eBT/SRT utilization trends by dermatologists, 2016–2021.

description: The state-level map demonstrates (A) the number of dermatologists utilizing eBT/SRT in 2021 and (B) the associated change in number of dermatologists utilizing eBT/SRT from 2016 to 2021. 

eBT = Electronic Brachytherapy; SRT = Superficial Radiotherapy
DOI: 10.17632/8xc7cj7z5v.1
title: Association of markers of intestinal inflammation and permeability with clinical manifestations of Parkinson's disease

description: This is a dataset for a paper in which markers of intestinal inflammation were examined in patients with Parkinson's disease and healthy controls. The values ​​of the markers were compared with the clinical parameters of the patient, such as the severity of motor and non-motor symptoms, sleep disorders and the like. The above information is attached.