cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.17632/r25wxy79dz.11
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/r25wxy79dz.12
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/r25wxy79dz.9
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c).
DOI: 10.17632/438b4xdws7.1
title: Data for: Plant species richness of alpine grasslands and their responses to different precipitation scenarios in Tibet

description: Site species richness and 20 environmental factors
DOI: 10.17632/52t2sdgcbt.1
title: Data for: Last Interglacial (MIS 5e) and Holocene paleohydrology and paleovegetation of midcontinental North America from Gulf of Mexico sediments

description: The supplementary material includes r2 values and p-values of the simple linear regressions between the past sea surface temperatures in the GOM and leaf wax isotopic compositions and ACL measured in ODP625B core. The supplementary table S1 includes plant wax concentration and isotopic compositions measured in ODP625B core.
DOI: 10.17632/84gndytbsm.1
title: Data for: Exploring the relationship between teacher enjoyment of mathematics, their attitudes towards student struggle and instructional time amongst early years primary teachers

description: Survey data from a sample of 102 teachers and teacher-leaders (Foundation to Year 2) from a professional learning day in Melbourne, Australia. Amongst other things, the data set captures teacher attitudes towards student struggle, teacher enjoyment of teaching mathematics and instructional time.
DOI: 10.17632/dtvvt9pc9c.1
title: NNA subsurface temperature response

description: Data used for plotting fig1-4.
DOI: 10.17632/p3kfkfvp95.1
title: Data for: Last Interglacial (MIS 5e) and Holocene paleohydrology and paleovegetation of midcontinental North America from Gulf of Mexico sediments

description: We performed a simple linear regression to investigate the correlation between the past sea surface temperatures (Ziegler et al., 2008) in the Gulf of Mexico and leaf wax isotopic compositions and average chain-length measured in ODP625B core.
DOI: 10.17632/r25wxy79dz.13
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/r25wxy79dz.14
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/r25wxy79dz.15
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/r25wxy79dz.16
title: Bastnäsite nanoparticles in carbonatite-syenite-hosted REE deposit

description: SEM images of the bastnäsite in the Maoniuping REE deposit, showing that bastnäsite is associated with fluorite (a). High magnification SEM images of the bastnäsite associated with fluorite (b). The SEM-EDS patterns of bastnäsite associated with fluorite, showing that F (c) and Ca (d) are mainly distributed in fluorite and La (e) and Ce (f) are mainly distributed in bastnäsite. Fl: fluorite; Bsa: bastnäsite. HRTEM image of bastnäsite (a), showing that nanoparticle is abundant in bastnäsite. The EDS image (b) and FFT pattern (c) showing small bastnäsite nanoparticles distributed in the outer surface of bastnäsite crystal. The EDS image (d) and FFT pattern (e) showing large nanoparticles distributed in the interior surface of bastnäsite crystal. The EDS image (f) and FFT pattern (g) showing the composition and lattice characteristics of bastnäsite crystal. Schematic illustration of the process of bastnäsite crystal via random attachment. Under external pressure (tectonic stress), growth and realignment of small nanoparticles occurred in the outer surface of bastnäsite crystal. The tectonic stress and the inherent surface stress induce realignment of large nanoparticles to form bastnäsite crystal. Lattice match was neither observed between the small bastnäsite nanoparticle and large bastnäsite nanoparticle nor between large bastnäsite nanoparticle and the main bastnäsite crystal demonstrate the random attachment pathway. Bastnäsite nanoparticles occurred in different bastnäsite mineral samples (M2-M6), indicating that bastnäsite nanoparticles are widely occurred in the Maoniuping REE deposit. Bastnäsite nanoparticles occurred in fluorite (a). The FFT patterns of bastnäsite nanoparticles (b) and fluorite (c). Table S1. EDS results (wt.%) of small bastnäsite nanoparticles Table S2. EDS results (wt.%) of large bastnäsite nanoparticles
DOI: 10.17632/9kwpzr67ms.1
title: management controls as a system

description: survey data
DOI: 10.17632/m6pny2w23t.1
title: Western Northern Luzon Isotopic Evidence of Transition from Proto-South China Sea to South China Sea Fossil Ridge Subduction

description: Text S1-3 present detailed sample description, analytical methods (Text S1), discussion on emplacement age of the Central Cordillera diorite complex (Text S2) and evaluation of post-magmatic alteration (Text S3) for the western Northern Luzon igneous rocks. The supporting figures provide 1) spatial variation of Sr isotope composition, 2) microphotographs, 3) zircon CL images, 4) plots of K2O and Sr-Nd-Pb isotope composition versus LOI, and 5) correlations between Sr-Nd isotope composition and silica for the western Northern Luzon igneous rocks. The supporting tables provide original data used in the main article.
DOI: 10.17632/m6pny2w23t.2
title: Western Northern Luzon Isotopic Evidence of Transition from Proto-South China Sea to South China Sea Fossil Ridge Subduction

description: Text S1-3 present detailed sample description, analytical methods (Text S1), discussion on emplacement age of the Central Cordillera diorite complex (Text S2) and evaluation of post-magmatic alteration (Text S3) for the western Northern Luzon igneous rocks. The supporting figures provide 1) spatial variation of Sr isotope composition, 2) microphotographs, 3) zircon CL images, 4) plots of K2O and Sr-Nd-Pb isotope composition versus LOI, and 5) correlations between Sr-Nd isotope composition and silica for the western Northern Luzon igneous rocks. The supporting tables provide original data used in the main article.
DOI: 10.5281/zenodo.3549924
title: 2016-10-23 │Tossal de Mortórum│ Proyecto gráfico y geomático

description: Proyecto gráfico y geomático del realizado por <strong>AD&D 4D</strong> para el proyecto web Castellón Arqueológico, patrocinada por la Diputación de Castellón. <strong>Yacimiento arqueológico</strong>: Tossal de Mortórum; Cabanes; Plana Alta, Castellón; Comunitat Valenciana; España; Europa Nube de puntos GeoRef 34 Millones de puntos (20161023MortorumNPD34M) DEM (Digital Elevation Model) GeoRef 1 cm / Pix (20161023MortorumDEM01cm) OrtofotoMapa GeoTiff 1 cm. / Pix (20161023MortorumOrto01cm) ETRS89 / UTM zona 31 (EPSG :: 25831) Visor 3D Sketchfab Más información: español. valenciano , inglés <strong>Fecha de captura: 2016-10-23</strong>
DOI: 10.5281/zenodo.3549925
title: 2016-10-23 │Tossal de Mortórum│ Proyecto gráfico y geomático

description: Proyecto gráfico y geomático del realizado por <strong>AD&D 4D</strong> para el proyecto web Castellón Arqueológico, patrocinada por la Diputación de Castellón. <strong>Yacimiento arqueológico</strong>: Tossal de Mortórum; Cabanes; Plana Alta, Castellón; Comunitat Valenciana; España; Europa Nube de puntos GeoRef 34 Millones de puntos (20161023MortorumNPD34M) DEM (Digital Elevation Model) GeoRef 1 cm / Pix (20161023MortorumDEM01cm) OrtofotoMapa GeoTiff 1 cm. / Pix (20161023MortorumOrto01cm) ETRS89 / UTM zona 31 (EPSG :: 25831) Visor 3D Sketchfab Más información: español. valenciano , inglés <strong>Fecha de captura: 2016-10-23</strong>
DOI: 10.17632/kjy66w8d8m.1
title: supplementary materials for study entitled "Water evolution and hydration kinetics of cement paste under steam-curing condition based on low-field NMR method"

description: The hydration rate of Portland cement pastes with different water to cement ratio during initial steam-curing cycle.
DOI: 10.17632/nw3p86dcrc.1
title: Archaea (for publication test)

description: DSA files of Archaea
DOI: 10.17632/3h7cj7gjvr.1
title: Collaborative DST-based TASK Pre- and Post-test data

description: This data represents the learning outcomes of the students taught before (pre-test) and after (post-test) the treatment using the collaborative Digital Storytelling-based task approach for the writing instruction.
DOI: 10.5281/zenodo.3550068
title: Diabetic Retinopathy Patient Survey Data

description: Patient survey data
DOI: 10.5281/zenodo.3550069
title: Diabetic Retinopathy Patient Survey Data

description: Patient survey data
DOI: 10.17632/kjy66w8d8m.2
title: supplementary materials for study entitled "Water evolution and hydration kinetics of cement paste under steam-curing condition based on low-field NMR method"

description: The hydration rate of Portland cement pastes with different water to cement ratio during initial steam-curing cycle.
DOI: 10.17632/b4vbtvx6gz.1
title: EDX OF UPPER LIMB

description: We collected data (demographic, clinical EDX, biochemical, psychometric) from patients regerred for Upper limb EDX studies and correlated them to EDX result. Our aim was to trace factors that might predict normal EDX result and investigate the reasons why women are more often referred than men for EDX studies.
DOI: 10.17632/hrdjzs6f28.1
title: Xuewei Hao-Appendix-Polycyclic aromatic hydrocarbon and nitro-polycyclic aromatic hydrocarbon emissions when crop residues are burned in domestic stoves in rural China

description: The Appendix of "Polycyclic aromatic hydrocarbon and nitro-polycyclic aromatic hydrocarbon emissions when crop residues are burned in domestic stoves in rural China"
DOI: 10.17632/kjy66w8d8m.3
title: Hydration rate of cement pastes during steam-curing process

description: The hydration rate of Portland cement pastes with different water to cement ratio during initial steam-curing cycle.
DOI: 10.17632/vdygnzprpw.1
title: Tertiary Study of MDE on software modeling characteristics

description: Data set for Systematic Reviews of MDE on software modeling characteristics.
DOI: 10.17632/bk448r8vfy.1
title: Cross-national dataset from Chile, Spain, Venezuela and Colombia to analyze the meanings students attribute to the pedagogical authority of teachers

description: This dataset includes the answers of 913 university students from 4 different Ibero-American countries (Spain, Chile, Colombia and Venezuela) to a set of questions related to the perception of teachers as authority figures. These questions constitute the 17 items that make up the Scale of Pedagogical Authority Meanings in the Classroom. As a result of the psychometric properties evaluation, a list of the components of each factor has been established: a) Closeness and Empathy (composed by 6 items): Being nice Teaching in an entertaining way Being cool Being friendly with students Being democratic in the classroom Having an outgoing personality b) Teaching and Respect (4 items) Teaching in a clear way Possessing a deep knowledge of the subject Being intelligent Being respectful with students c) Gender of the teacher (2 items) Being a woman Being a man d) Character, Demand and Experience (4 items) Possessing much professional experience Having a strong character Teaching an important subject Applying sanctions relentlessly