cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.10251595
title: Data and Codes for "Graphene-Based Quantum Hall Interferometer with Self-Aligned Side Gates"

description: Data and Codes for "Graphene-Based Quantum Hall Interferometer with Self-Aligned Side Gates"
description: Transport measurements conducted by L.Z., E.G.A., and T.F.Q.L. were supported by NSF award DMR-2004870. Lithographic fabrication and characterization of the samples by L.Z. and A.S., as well as the project guidence by Z.I. and G.F., were supported by the Division of Materials Sciences and Engineering, Office of Basic Energy Sciences, U.S. Department of Energy, under Award No. DE-SC0002765. T.F. and F.A. were supported by a URC grant at Appalachian State University. K.W. and T.T. acknowledge support from the Elemental Strategy Initiative conducted by the MEXT, Japan (grant no. JPMXP0112101001), JSPS KAKENHI (grant no. JP20H00354), and CREST (no. JPMJCR15F3, JST). The sample fabrication was performed in part at the Duke University Shared Materials Instrumentation Facility (SMIF), a member of the North Carolina Research Triangle Nanotechnology Network (RTNN), which is supported by the National Science Foundation (Grant ECCS-1542015) as part of the National Nanotechnology Coordinated Infrastructure (NNCI).
DOI: 10.5281/zenodo.10251596
title: Data and Codes for "Graphene-Based Quantum Hall Interferometer with Self-Aligned Side Gates"

description: Data and Codes for "Graphene-Based Quantum Hall Interferometer with Self-Aligned Side Gates"
description: Transport measurements conducted by L.Z., E.G.A., and T.F.Q.L. were supported by NSF award DMR-2004870. Lithographic fabrication and characterization of the samples by L.Z. and A.S., as well as the project guidence by Z.I. and G.F., were supported by the Division of Materials Sciences and Engineering, Office of Basic Energy Sciences, U.S. Department of Energy, under Award No. DE-SC0002765. T.F. and F.A. were supported by a URC grant at Appalachian State University. K.W. and T.T. acknowledge support from the Elemental Strategy Initiative conducted by the MEXT, Japan (grant no. JPMXP0112101001), JSPS KAKENHI (grant no. JP20H00354), and CREST (no. JPMJCR15F3, JST). The sample fabrication was performed in part at the Duke University Shared Materials Instrumentation Facility (SMIF), a member of the North Carolina Research Triangle Nanotechnology Network (RTNN), which is supported by the National Science Foundation (Grant ECCS-1542015) as part of the National Nanotechnology Coordinated Infrastructure (NNCI).
DOI: 10.5281/zenodo.3708373
title: Data and Codes for "Interference of chiral Andreev edge states"

description: Source data, analysis codes and simulation codes for "Interference of chiral Andreev edge states"
DOI: 10.5281/zenodo.3708374
title: Data and Codes for "Interference of chiral Andreev edge states"

description: Source data, analysis codes and simulation codes for "Interference of chiral Andreev edge states"
DOI: 10.48597/cfpm-wxud
title: Measurement of Particle_number_concentration at Whistler Mountain

description: Measurement of Particle_number_concentration at Whistler Mountain
DOI: 10.5281/zenodo.8332180
title: Experimental determination of alumina solubility in periclase to lower mantle conditions

description: This dataset includes the tables displayed in the manuscript and the scripts of the thermodynamic model of the MgO-Al<sub>2</sub>O<sub>3</sub> solid solution.
DOI: 10.5281/zenodo.10828212
title: Dataset presented in "Alumina solubility in periclase determined to lower mantle conditions and implications for ferropericlase inclusions in diamonds"

description: This dataset includes the tables displayed in the manuscript, the scripts of the thermodynamic model of the MgO-Al2O3 solid solution, and a spreadsheet to calculate Al2O3 solubility in periclase.
DOI: 10.5281/zenodo.8290097
title: Dataset presented in "Alumina solubility in periclase determined to lower mantle conditions and implications for ferropericlase inclusions in diamonds"

description: This dataset includes the tables displayed in the manuscript, the scripts of the thermodynamic model of the MgO-Al2O3 solid solution, and a spreadsheet to calculate Al2O3 solubility in periclase.
DOI: 10.5281/zenodo.8290098
title: Alumina solubility in periclase determined to lower mantle conditions: A novel thermometer for high-pressure experiments and diamond inclusions

description: This dataset includes the data of periclase compositions and spatial distribution used for Fig.5 and Fig. 6 and the scripts of the thermodynamic model of the MgO-Al<sub>2</sub>O<sub>3</sub> solid solution.
DOI: 10.5281/zenodo.8299521
title: Alumina solubility in periclase determined to lower mantle conditions: A novel thermometer for high-pressure experiments and diamond inclusions

description: This dataset includes the data of periclase compositions and spatial distribution used for Fig.4 and Fig. 5 and the scripts of the thermodynamic model of the MgO-Al<sub>2</sub>O<sub>3</sub> solid solution.
DOI: 10.5281/zenodo.8388962
title: Dataset presented in "Alumina solubility in periclase determined to lower mantle conditions and implications for ferropericlase inclusions in diamonds"

description: This dataset includes the tables displayed in the manuscript and the scripts of the thermodynamic model of the MgO-Al<sub>2</sub>O<sub>3</sub> solid solution.
DOI: 10.6084/m9.figshare.25425913.v1
title: Data from "BREEDING BIRD COMMUNITIES OF RIPARIAN AND UPLAND WOODLANDS RESPOND DIFFERENTLY TO AN ATLANTIC-MEDITERRANEAN CLIMATIC GRADIENT IN MAINLAND SPAIN"

description: Original data in Excel from a manuscript where the first sheet shows the meaning of each of the variables that occur in the second sheet.
DOI: 10.6084/m9.figshare.25425913
title: Data from "BREEDING BIRD COMMUNITIES OF RIPARIAN AND UPLAND WOODLANDS RESPOND DIFFERENTLY TO AN ATLANTIC-MEDITERRANEAN CLIMATIC GRADIENT IN MAINLAND SPAIN"

description: Original data in Excel from a manuscript where the first sheet shows the meaning of each of the variables that occur in the second sheet.
DOI: 10.5281/zenodo.10732214
title: Tsunami Deposits in the Guerrero Seismic Gap, Mexico: Insights from Location Analysis, Earthquake and Tsunami Models, and Proxy Dataset

description: Globally, the most significant tsunamigenic earthquakes have occurred along subduction zones. Catastrophic events surpassing magnitude 9, such as those witnessed in Chile, Sumatra, and Japan, have occurred in regions where instrumental records of similar events are lacking. Despite the absence of such occurrences along the 1000-kilometer-long Mexican subduction zone, historical and geological evidence strongly suggests the likelihood of a magnitude 8.6 tsunamigenic earthquake. However, the Guerrero seismic gap has remained devoid of high-magnitude earthquakes for over a century. In this study, we present findings from analyses of sediment grain size, geochemistry, microfossils, magnetic properties, and radiometric and optically stimulated luminescence dating conducted along the Guerrero coast. Our research provides compelling evidence of a 2000-year history of significant tsunamis triggered by potentially large earthquakes. Numerical modeling reinforces our conclusions, pointing to a magnitude >8 event occurring around the year 1300 in the Guerrero seismic gap. This evidence underscores the critical importance of evaluating earthquake and tsunami potential through long-term evidence and instrumental observations along subduction zones globally. Additionally, this dataset includes the locations of study sites, proxy data, and earthquake and tsunami models.

Source data:



Grain size - Figure S1

Geochemical - Figure S2

Maximum tsunami wave amplitude - Figure 3d and S4

Maximum tsunami wave amplitude - Figure S5c
DOI: 10.5281/zenodo.10732215
title: Tsunami Deposits in the Guerrero Seismic Gap, Mexico: Insights from Location Analysis, Earthquake and Tsunami Models, and Proxy Dataset

description: Globally, the most significant tsunamigenic earthquakes have occurred along subduction zones. Catastrophic events surpassing magnitude 9, such as those witnessed in Chile, Sumatra, and Japan, have occurred in regions where instrumental records of similar events are lacking. Despite the absence of such occurrences along the 1000-kilometer-long Mexican subduction zone, historical and geological evidence strongly suggests the likelihood of a magnitude 8.6 tsunamigenic earthquake. However, the Guerrero seismic gap has remained devoid of high-magnitude earthquakes for over a century. In this study, we present findings from analyses of sediment grain size, geochemistry, microfossils, magnetic properties, and radiometric and optically stimulated luminescence dating conducted along the Guerrero coast. Our research provides compelling evidence of a 2000-year history of significant tsunamis triggered by potentially large earthquakes. Numerical modeling reinforces our conclusions, pointing to a magnitude >8 event occurring around the year 1300 in the Guerrero seismic gap. This evidence underscores the critical importance of evaluating earthquake and tsunami potential through long-term evidence and instrumental observations along subduction zones globally. Additionally, this dataset includes the locations of study sites, proxy data, and earthquake and tsunami models.

Source data:



Grain size - Figure S1

Geochemical - Figure S2

Maximum tsunami wave amplitude - Figure 3d and S4

Maximum tsunami wave amplitude - Figure S5c
DOI: 10.6084/m9.figshare.25425963
title: Raw data from Surviving the heat: the thermal tolerance of a keystone ecosystem engineer is hampered by microplastic leachates from The tolerance of a keystone ecosystem engineer to extreme heat stress is hampered by microplastic leachates

description: Raw data used in Surviving the heat: the thermal tolerance of a keystone ecosystem engineer is hampered by microplastic leachates
DOI: 10.6084/m9.figshare.25425963.v1
title: Raw data from Surviving the heat: the thermal tolerance of a keystone ecosystem engineer is hampered by microplastic leachates from The tolerance of a keystone ecosystem engineer to extreme heat stress is hampered by microplastic leachates

description: Raw data used in Surviving the heat: the thermal tolerance of a keystone ecosystem engineer is hampered by microplastic leachates
DOI: 10.17632/jf7k2g5cdy.1
title: Supplement for Comparative Long-Term Efficacy of Phenol-Croton Oil Chemical Peels for Persistent Melasma at Varied Croton tiglium Oil Concentrations

description: Files: 
Figures Supplement.pdf: Figures S1-S4 (Clinical and Histological Evolution)
Supplement Dataset.xlsx: Raw Dataset of the JAAD research letter.
DOI: 10.6084/m9.figshare.25425979.v1
title: Untitled Item

description: Table S4 for reviewers to dicuss.
DOI: 10.6084/m9.figshare.25425979
title: Untitled Item

description: Table S4 for reviewers to dicuss.
DOI: 10.6084/m9.figshare.25406173
title: Elsafty_RBCs_Slide_10

description: Each one of (Elsafty_RBCs_Slide_1-25) contains the field images/patches of a specific slide/patient. The names of the patches start with the respective slide/patient number, followed by the unique patch/field number. There is a total of 47,363 patches with 1076x535 pixels size from the 25 slides/patients, the counts of patches per slide/patient are as follows: 1690, 1709, 2697, 2400, 1905, 1803, 2964, 3049, 2464, 2080, 1894, 1852, 2590, 2263, 3328, 983, 1066, 935, 1131, 1237, 1874, 1393, 1277, 1199, and 1580.
DOI: 10.6084/m9.figshare.25406185
title: Elsafty_RBCs_Slide_11

description: Each one of (Elsafty_RBCs_Slide_1-25) contains the field images/patches of a specific slide/patient. The names of the patches start with the respective slide/patient number, followed by the unique patch/field number. There is a total of 47,363 patches with 1076x535 pixels size from the 25 slides/patients, the counts of patches per slide/patient are as follows: 1690, 1709, 2697, 2400, 1905, 1803, 2964, 3049, 2464, 2080, 1894, 1852, 2590, 2263, 3328, 983, 1066, 935, 1131, 1237, 1874, 1393, 1277, 1199, and 1580.
DOI: 10.6084/m9.figshare.25425985
title: Untitled Item

description: Table S4 - ONLY for reviewer!
DOI: 10.6084/m9.figshare.25425985.v1
title: Untitled Item

description: Table S4 - ONLY for reviewer!
DOI: 10.6084/m9.figshare.23939449
title: Evolved Late Mesozoic continental arc: Constraints of detrital zircons from the western East China Sea

description: The Late Mesozoic subduction of Izanagi slab beneath East Asia formed large-scale intraplate magmatism in SE South China and subduction mélanges outcropped in SW Japan to eastern Taiwan Island, but the accompanying arc remains uncertain. We conducted LA-ICP-MS U–Pb zircon dating and trace element analyses of proximal sandstones from the SW East China Sea to trace a Jurassic to Cretaceous magmatic arc. Newly acquired data reveal that arc magmatism mostly developed in episodes of 150–124 and 124–102 Ma, exhibiting characteristics of low-<i>T</i>, high Th/U, U/Yb, Sc/Yb, Th/Nb, and low Nb/Yb, Nb/Hf ratios. This magmatic arc, combined with the SE South China intraplate and residual subduction mélanges, spatially forms a Late Mesozoic trench–arc–intraplate architecture responding to the Izanagi subduction. Its identified tectonic scenarios mainly include slab strike-slip subduction (200–170 Ma), slab stagnation and intraplate foundering (170–150 Ma), slab rollback and arc-root removal (150–102 Ma), and arc migration (102–86 Ma). Both the western East China Sea and Cathaysia block share a unified Paleoproterozoic basement that formed at ca. 1.85 Ga, and the Cathaysia-based magmatic arc occurred then.
DOI: 10.6084/m9.figshare.23832921.v1
title: An evolving tectonic environment of Early to Middle Permian granitic plutons in the Barkol area, East Junggar: insights from integrated zircon U–Pb ages, geochemistry, and Nd–Sr–Hf isotopes

description: Located in the central part of the Central Asian Orogenic Belt, East Junggar represents one of the most important sites of juvenile crustal growth during the Phanerozoic. However, the mechanism of juvenile crustal growth during the Permian remains controversial. The Daheishan granites in the eastern segment of East Junggar are dated at ~292 Ma (Early Permian) and 269 Ma–267 Ma (Middle Permian). The Early Permian granites are coarse-grained with very high SiO<sub>2</sub> (76.64 wt%–80.02 wt%), Al<sub>2</sub>O<sub>3</sub> (10.72 wt%–12.96 wt%), and K<sub>2</sub>O/Na<sub>2</sub>O (1.27‒2.14), and low TiO<sub>2</sub> (0.12 wt%–0.18 wt%), CaO (0.27 wt%–0.90 wt%), Mg# (25–32), and Sr/Yb (16–25). The Middle Permian granites are medium‒fine-grained with relatively high SiO<sub>2</sub> (71.84 wt%–76.26 wt%), Al<sub>2</sub>O<sub>3</sub> (11.26 wt%–13.00 wt%), and K<sub>2</sub>O/Na<sub>2</sub>O (0.53–1.54), and low TiO<sub>2</sub> (0.17 wt%–0.21 wt%), CaO (0.37 wt%–3.20 wt%), Mg# (33–43), and Sr/Yb (5–9). These Permian granites display slightly positive whole-rock εNd(t) (+0.77 to + 1.04) and highly positive zircon εHf(t) (+7.3 to + 8.7) values, and low Ga/Al (2.04–2.55 &lt; 2.6), P<sub>2</sub>O<sub>5</sub> (0.02%–0.05% &lt;0.14%), and zircon saturation temperature (690°C–749°C, take the median for each sample). Moreover, they display characteristic tetrad rare earth element patterns and non-CHARAC (CHArge-and-RAdius-Controlled) trace element behaviour, suggesting that the Daheishan granites are I-type granites that underwent both fractional crystallization (K-feldspar and plagioclase, e.g.) and crustal contamination prior to their emplacement. In combination with data from volcanic rocks in the Santanghu Basin, we infer that the Early Permian granitic magmas were derived from delamination of a thickened lithospheric mantle base and partial melting of pre-Permian arc components, while the Middle Permian granites formed during the subsequent stretching and thinning of the lithosphere.
DOI: 10.6084/m9.figshare.23931633.v1
title: Origins of magmatism in the Okinawa Trough: Fe–Sr–Nd–Pb–Hf isotopic constraints

description: The Okinawa Trough is an incipient back-arc basin formed by the subduction of the Philippine Sea Plate beneath the Eurasian Plate and is a natural laboratory for studying basin evolution, magmatism, and crust-mantle interactions during the early stages of back-arc spreading. Back-arc spreading and recent magmatism are occurring mainly in the Middle Okinawa Trough (MOT) and Southern Okinawa Trough (SOT). In order to investigate the magmatism in the Okinawa Trough, volcanic rock samples from the MOT and SOT were analysed for Fe – Sr – Nd – Pb – Hf isotopic compositions. The Fe isotopic compositions of basaltic andesite samples from the SOT are similar to or lower than MORBs. The fluid/melt derived from the subducted slab, especially the fluid dehydrated from slab serpentinites and sediment-derived melts, entered the overlying depleted mantle wedge and participated in magma generation, which resulted in the low δ<sup>56</sup>Fe values of the SOT basaltic magmas. The δ<sup>56</sup>Fe values of volcanic rocks from the MOT increase with increasing SiO<sub>2</sub> contents, suggesting a gradual enrichment of heavy Fe isotopes during the evolution of the magma as it ascended to the surface. While the Sr – Nd – Pb – Hf isotopic compositions do not vary significantly, suggesting that the different samples are the products of different degrees of crystal fractionation of comagma. The fractional crystallization of olivine, pyroxene, and ilmenite minerals, which enrich in light Fe isotopes, resulted in the gradual increase in Fe isotopic values of magma during its evolution. The dacites and rhyolites from the southernmost Okinawa Trough have the similar δ<sup>56</sup>Fe values with the basaltic andesite and the basalt from the SOT and MOT, accompanied by significantly lower Nd and Hf isotope ratios relative to basalts, reflecting that the contamination of crustal materials would not change the magma in Fe isotope compositions evidently. Compared with the MOT, the volcanic rocks from the SOT was more affected by subduction components on their underlying mantle, and those from the southernmost experienced more contamination by crustal materials in the evolving magma.
DOI: 10.6084/m9.figshare.23832921
title: An evolving tectonic environment of Early to Middle Permian granitic plutons in the Barkol area, East Junggar: insights from integrated zircon U–Pb ages, geochemistry, and Nd–Sr–Hf isotopes

description: Located in the central part of the Central Asian Orogenic Belt, East Junggar represents one of the most important sites of juvenile crustal growth during the Phanerozoic. However, the mechanism of juvenile crustal growth during the Permian remains controversial. The Daheishan granites in the eastern segment of East Junggar are dated at ~292 Ma (Early Permian) and 269 Ma–267 Ma (Middle Permian). The Early Permian granites are coarse-grained with very high SiO<sub>2</sub> (76.64 wt%–80.02 wt%), Al<sub>2</sub>O<sub>3</sub> (10.72 wt%–12.96 wt%), and K<sub>2</sub>O/Na<sub>2</sub>O (1.27‒2.14), and low TiO<sub>2</sub> (0.12 wt%–0.18 wt%), CaO (0.27 wt%–0.90 wt%), Mg# (25–32), and Sr/Yb (16–25). The Middle Permian granites are medium‒fine-grained with relatively high SiO<sub>2</sub> (71.84 wt%–76.26 wt%), Al<sub>2</sub>O<sub>3</sub> (11.26 wt%–13.00 wt%), and K<sub>2</sub>O/Na<sub>2</sub>O (0.53–1.54), and low TiO<sub>2</sub> (0.17 wt%–0.21 wt%), CaO (0.37 wt%–3.20 wt%), Mg# (33–43), and Sr/Yb (5–9). These Permian granites display slightly positive whole-rock εNd(t) (+0.77 to + 1.04) and highly positive zircon εHf(t) (+7.3 to + 8.7) values, and low Ga/Al (2.04–2.55 &lt; 2.6), P<sub>2</sub>O<sub>5</sub> (0.02%–0.05% &lt;0.14%), and zircon saturation temperature (690°C–749°C, take the median for each sample). Moreover, they display characteristic tetrad rare earth element patterns and non-CHARAC (CHArge-and-RAdius-Controlled) trace element behaviour, suggesting that the Daheishan granites are I-type granites that underwent both fractional crystallization (K-feldspar and plagioclase, e.g.) and crustal contamination prior to their emplacement. In combination with data from volcanic rocks in the Santanghu Basin, we infer that the Early Permian granitic magmas were derived from delamination of a thickened lithospheric mantle base and partial melting of pre-Permian arc components, while the Middle Permian granites formed during the subsequent stretching and thinning of the lithosphere.
DOI: 10.6084/m9.figshare.23931633
title: Origins of magmatism in the Okinawa Trough: Fe–Sr–Nd–Pb–Hf isotopic constraints

description: The Okinawa Trough is an incipient back-arc basin formed by the subduction of the Philippine Sea Plate beneath the Eurasian Plate and is a natural laboratory for studying basin evolution, magmatism, and crust-mantle interactions during the early stages of back-arc spreading. Back-arc spreading and recent magmatism are occurring mainly in the Middle Okinawa Trough (MOT) and Southern Okinawa Trough (SOT). In order to investigate the magmatism in the Okinawa Trough, volcanic rock samples from the MOT and SOT were analysed for Fe – Sr – Nd – Pb – Hf isotopic compositions. The Fe isotopic compositions of basaltic andesite samples from the SOT are similar to or lower than MORBs. The fluid/melt derived from the subducted slab, especially the fluid dehydrated from slab serpentinites and sediment-derived melts, entered the overlying depleted mantle wedge and participated in magma generation, which resulted in the low δ<sup>56</sup>Fe values of the SOT basaltic magmas. The δ<sup>56</sup>Fe values of volcanic rocks from the MOT increase with increasing SiO<sub>2</sub> contents, suggesting a gradual enrichment of heavy Fe isotopes during the evolution of the magma as it ascended to the surface. While the Sr – Nd – Pb – Hf isotopic compositions do not vary significantly, suggesting that the different samples are the products of different degrees of crystal fractionation of comagma. The fractional crystallization of olivine, pyroxene, and ilmenite minerals, which enrich in light Fe isotopes, resulted in the gradual increase in Fe isotopic values of magma during its evolution. The dacites and rhyolites from the southernmost Okinawa Trough have the similar δ<sup>56</sup>Fe values with the basaltic andesite and the basalt from the SOT and MOT, accompanied by significantly lower Nd and Hf isotope ratios relative to basalts, reflecting that the contamination of crustal materials would not change the magma in Fe isotope compositions evidently. Compared with the MOT, the volcanic rocks from the SOT was more affected by subduction components on their underlying mantle, and those from the southernmost experienced more contamination by crustal materials in the evolving magma.