cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/ccdc.csd.cc21gm5b
title: CCDC 1890881: Experimental Crystal Structure Determination

description: Related Article: Ming Chen, Jing Li, Xuechen Jiao, Xiaochun Yang, Wenting Wu, Christopher R. McNeill, Xike Gao|2019|J.Mater.Chem.C|7|2659|doi:10.1039/C8TC06273K
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.17632/rhjr3czc9k.1
title: Data for: Ozone impact on wheat in Europe, Asia and North America - a comparison

description: Data extracted from the scientific literature to compare ozone sensitivity in wheat on different continents.
DOI: 10.17632/v92kyyknjx.1
title: Data for: The cross-section of returns in frontier equity markets: Integrated or segmented pricing?

description: The file contains the returns on asset pricing factors used in the study.
DOI: 10.26186/5c638c9dc5604
title: Geology of the Bunger Hills-Denman Glacier region, East Antarctica

description: The Bunger Hills area, which forms part of the East Antarctic Shield, consists predominantly of 
granulite facies orthogneiss (pyroxene-quartz-feldspar gneiss), with subordinate maficgranulite and garnet, sillimanite, and 
cordierite-bearing paragneiss. The igneous precursors of granodioritic orthogneiss crystallised about 1500 - 1700 Ma ago, 
whereas late Archaean (2640 Ma) tonalitic orthogneiss occurs in the Obruchev Hills, in the southwest of the area. Metamorphism 
reached a peak of about 750 - 800 Â° C and 5 - 6 kb (Mj) 1190Â±15 Ma ago (U-Pb zircon age) and was accompanied by the first of 
three ductile deformation events (Dj). Voluminous, mainly mantle-derived plutonic rocks were emplaced between 1170 (during D 3 ) 
and 1150 Ma. They range in composition from gabbro, through quartz gabbro, quartz monzogabbro, and quartz monzodiorite, to granite.
 Abundant dolerite dykes, of at least four chemically distinct groups, were intruded at about 1140 Ma. Their intrusion was associated 
 with the formation of shear zones, indicating at least limited uplift; all subsequent deformation was of brittle-ductile or brittle 
 type. Alkaline mafic dykes were emplaced 500 Ma ago. Marked geochronological similarities with the Albany Mobile Belt of Western 
 Australia suggest that high-grade metamorphism in both areas was the result of continental collision between the Archaean Yilgarn 
 Craton of Australia and the East Antarctic Shield. However, Gondwana reconstructions and the composition of the plutonic rocks 
 suggest that the Bunger Hills metamorphics may have formed in an Andean-type continental arc, with the actual collision zone 
 having been to the east of the present Bunger Hills. Exposures west of the Denman Glacier are also mainly granulite-facies 
 gneiss, intruded by a variety of mafic to felsic plutonic rocks. They differ from the Bunger Hills in being partly derived 
 from Archaean protoliths (- 3000 Ma), in lacking isotopic evidence for a Mesoproterozoic high-grade event, and in not being 
 intruded by dolerite dyke swarms. They also show evidence of much more extensive 500 - 600 M a (Pan-African) metamorphism 
 and plutonism (syenite to granite), and in this regard they are comparable with the Leeuwin Block metamorphics of southwestern 
 Australia, although these were derived from significantly younger protoliths (T^D  model ages: 1100 - 1500 Ma). If this early 
 Palaeozoic activity was also a consequence of continental collision, it would explain the markedly different geological history 
 of the terranes on either side of the Denman Glacier and could account for the final uplift of the Bunger Hills. However, the 
 compressional tectonic regime implicit in the collision hypothesis was followed by an extensional regime, which, in southwestern 
 Australia, eventually resulted in the formation of the Perth Basin rift zone. This structure is aligned with the Denman Glacier 
 trough on our preferred Gondwana reconstruction, suggesting that it may have extended well to the south before the breakup of 
 Gondwana.
DOI: 10.5281/zenodo.2558319
title: Data for: Holocene sedimentary record and coastal evolution in the Makran subduction zone (Iran)

description: The data comes from the study of Holocene beaches from the Iranian Makran. More exactly, the beaches in Pozm bay, Chabahar bay and the longitudinal beach west of the village of Beris. The data contain field pictures and their legends, results and analytical details of radiocarbon dating, SEM secondary electron images of the analysed shells and the results and analytical details of optically stimulated luminescence dating (OSL).<br>
The data is published in support for the paper mentioned in the title.

A to D are field pictures and legends of:<br>
A - Pozm bay field pictures<br>
B - Chabahar bay field pictures<br>
C - Beris beach field pictures<br>
D - Observed current depositional settings

E - Radiocarbon dating results and analytical supplementary information<br>
F - Secondary electrons SEM images of the analysed shells

G - OSL dating results and analytical supplementary information

Radiocarbon analytical details are provided, together with XRD analysis of the Aragonitic shells, SEM secondary electron images of analysed shells and calibration details. Method details are in the paper.

OSL results are provided with the analytical details, such as: Environmental dose parameters, OSL raw measurements (out of the machine), OSL Histograms and Dose-Recovery tests. Method details are in the paper.
DOI: 10.5281/zenodo.2558320
title: Data for: Holocene sedimentary record and coastal evolution in the Makran subduction zone (Iran)

description: The data comes from the study of Holocene beaches from the Iranian Makran. More exactly, the beaches in Pozm bay, Chabahar bay and the longitudinal beach west of the village of Beris. The data contain field pictures and their legends, results and analytical details of radiocarbon dating, SEM secondary electron images of the analysed shells and the results and analytical details of optically stimulated luminescence dating (OSL).<br>
The data is published in support for the paper mentioned in the title.

A to D are field pictures and legends of:<br>
A - Pozm bay field pictures<br>
B - Chabahar bay field pictures<br>
C - Beris beach field pictures<br>
D - Observed current depositional settings

E - Radiocarbon dating results and analytical supplementary information<br>
F - Secondary electrons SEM images of the analysed shells

G - OSL dating results and analytical supplementary information

Radiocarbon analytical details are provided, together with XRD analysis of the Aragonitic shells, SEM secondary electron images of analysed shells and calibration details. Method details are in the paper.

OSL results are provided with the analytical details, such as: Environmental dose parameters, OSL raw measurements (out of the machine), OSL Histograms and Dose-Recovery tests. Method details are in the paper.
DOI: 10.5281/zenodo.2558348
title: Data for: Pleistocene coastal evolution of the Makran subduction zone

description: This dataset contain a set of field pictures made along the coast of the western Makran subduction zone, near the region of Chabahar.<br>
A youtube video (diaporama) presents (some of) these figures in their context. https://www.youtube.com/watch?v=VRxXaCPRoJk&t=1s

The field pictures are a visual support for the publication mentioned in the title.

The dataset comes in the form of many field pictures classified in themes, their legends in text files and geolocalisation in a .kmz file.<br>
BB and HB are bay beach and headland beach pictures, respectively<br>
Pictures of the different marine terraces areas visited are labelled as follow:<br>
CH - Chabahar marine terraces<br>
GU - Gurdim marine terrace<br>
JA - Jask marine terrace<br>
KO - Konarak marine terraces<br>
LI - Lipar marine terraces<br>
PA - Pasabander marine terraces<br>
RA - Ramin marine terraces<br>
TA - Tang marine terraces

M pictures are from tertiary marl bedrock outcrops along the coast

Pictures B, C, D, E, F, G, and I are from major normal faults at Chabahar headland. A figure shows their localisation.

Finally, many pictures illustrate the different sedimentary sections described and studied in the paper.
DOI: 10.5281/zenodo.2558349
title: Data for: Pleistocene coastal evolution of the Makran subduction zone

description: This dataset contain a set of field pictures made along the coast of the western Makran subduction zone, near the region of Chabahar.<br>
A youtube video (diaporama) presents (some of) these figures in their context. https://www.youtube.com/watch?v=VRxXaCPRoJk&t=1s

The field pictures are a visual support for the publication mentioned in the title.

The dataset comes in the form of many field pictures classified in themes, their legends in text files and geolocalisation in a .kmz file.<br>
BB and HB are bay beach and headland beach pictures, respectively<br>
Pictures of the different marine terraces areas visited are labelled as follow:<br>
CH - Chabahar marine terraces<br>
GU - Gurdim marine terrace<br>
JA - Jask marine terrace<br>
KO - Konarak marine terraces<br>
LI - Lipar marine terraces<br>
PA - Pasabander marine terraces<br>
RA - Ramin marine terraces<br>
TA - Tang marine terraces

M pictures are from tertiary marl bedrock outcrops along the coast

Pictures B, C, D, E, F, G, and I are from major normal faults at Chabahar headland. A figure shows their localisation.

Finally, many pictures illustrate the different sedimentary sections described and studied in the paper.
DOI: 10.5281/zenodo.2559479
title: Data for: Extention at the coast of the Makran subduction zone (Iran)

description: This dataset comes from the study of normal faults at the coast of the Iranian Makran, near the city of Chabahar. The data is published in support for the paper mentioned in the title.

The dataset contains:<br>
A - A series of fault measurements made in the region of Chabahar, with the following subgroups:<br>
a) Major Faults of Chabahar headland, b) minor faults of Chabahar headland, c) faults measured from the Konarak headland, d) faults measured in the Parak area, in the Makran ranges north of Chabahar, e) Bedrock bedding orientations.

B - Shapefiles and KMZ file containing the structural measurements in A.

C - Field pictures of normal faults and observed evidence of overpressure in Tertiary sediments.
DOI: 10.5281/zenodo.2559480
title: Data for: Extention at the coast of the Makran subduction zone (Iran)

description: This dataset comes from the study of normal faults at the coast of the Iranian Makran, near the city of Chabahar. The data is published in support for the paper mentioned in the title.

The dataset contains:<br>
A - A series of fault measurements made in the region of Chabahar, with the following subgroups:<br>
a) Major Faults of Chabahar headland, b) minor faults of Chabahar headland, c) faults measured from the Konarak headland, d) faults measured in the Parak area, in the Makran ranges north of Chabahar, e) Bedrock bedding orientations.

B - Shapefiles and KMZ file containing the structural measurements in A.

C - Field pictures of normal faults and observed evidence of overpressure in Tertiary sediments.
DOI: 10.26186/5c638cd2a20a0
title: Geology of the Bunger Hills-Denman Glacier region, East Antarctica

description: The Bunger Hills area, which forms part of the East Antarctic Shield, consists predominantly of 
granulite facies orthogneiss (pyroxene-quartz-feldspar gneiss), with subordinate maficgranulite and garnet, sillimanite, and 
cordierite-bearing paragneiss. The igneous precursors of granodioritic orthogneiss crystallised about 1500 - 1700 Ma ago, 
whereas late Archaean (2640 Ma) tonalitic orthogneiss occurs in the Obruchev Hills, in the southwest of the area. Metamorphism 
reached a peak of about 750 - 800 Â° C and 5 - 6 kb (Mj) 1190Â±15 Ma ago (U-Pb zircon age) and was accompanied by the first of 
three ductile deformation events (Dj). Voluminous, mainly mantle-derived plutonic rocks were emplaced between 1170 (during D 3 ) 
and 1150 Ma. They range in composition from gabbro, through quartz gabbro, quartz monzogabbro, and quartz monzodiorite, to granite.
 Abundant dolerite dykes, of at least four chemically distinct groups, were intruded at about 1140 Ma. Their intrusion was associated 
 with the formation of shear zones, indicating at least limited uplift; all subsequent deformation was of brittle-ductile or brittle 
 type. Alkaline mafic dykes were emplaced 500 Ma ago. Marked geochronological similarities with the Albany Mobile Belt of Western 
 Australia suggest that high-grade metamorphism in both areas was the result of continental collision between the Archaean Yilgarn 
 Craton of Australia and the East Antarctic Shield. However, Gondwana reconstructions and the composition of the plutonic rocks 
 suggest that the Bunger Hills metamorphics may have formed in an Andean-type continental arc, with the actual collision zone 
 having been to the east of the present Bunger Hills. Exposures west of the Denman Glacier are also mainly granulite-facies 
 gneiss, intruded by a variety of mafic to felsic plutonic rocks. They differ from the Bunger Hills in being partly derived 
 from Archaean protoliths (- 3000 Ma), in lacking isotopic evidence for a Mesoproterozoic high-grade event, and in not being 
 intruded by dolerite dyke swarms. They also show evidence of much more extensive 500 - 600 M a (Pan-African) metamorphism 
 and plutonism (syenite to granite), and in this regard they are comparable with the Leeuwin Block metamorphics of southwestern 
 Australia, although these were derived from significantly younger protoliths (T^D  model ages: 1100 - 1500 Ma). If this early 
 Palaeozoic activity was also a consequence of continental collision, it would explain the markedly different geological history 
 of the terranes on either side of the Denman Glacier and could account for the final uplift of the Bunger Hills. However, the 
 compressional tectonic regime implicit in the collision hypothesis was followed by an extensional regime, which, in southwestern 
 Australia, eventually resulted in the formation of the Perth Basin rift zone. This structure is aligned with the Denman Glacier 
 trough on our preferred Gondwana reconstruction, suggesting that it may have extended well to the south before the breakup of 
 Gondwana.
DOI: 10.7910/dvn/mtawhx
title: Replication data for: Decennial Gold & Silver Registrations

description: Decennial Gold & Silver Registrations, 1492-1810: Caribbean, Mexico, Central America, New Granada, Ecuador, Peru (Lower & Upper), Chile, Río de la Plata, Brazil; in pesos & kilograms; including regional percentage share & percentage change; summaries by North & South American.
DOI: 10.6092/unibo/amsacta/6101
title: Mid Adriatic Deep Dataset

description: This dataset is part of an ongoing larger project that aims to build a comprehensive macrobenthic dataset from the Po Plain‒Adriatic Sea system by sampling both sedimentary successions and present-day depositional surfaces. During my Ph.D. research, I processed samples taken from the Mid Adriatic Deep (MAD) and near-MAD cored sedimentary succession in the central Adriatic, that contain marine lowstand deltaic and costal deposits from the last glacial time interval. Although an abundance of data has been gathered from the sedimentary succession of the Adriatic Sea, the dynamics of the macrobenthic community preserved there has been little investigated. The taxonomic and ecological information reported in the MAD dataset will represent a keystone for enhancing the knowledge of the molluscan fauna during the last glacial period.
DOI: 10.7910/dvn/gcuulv
title: Replication data for: Silver Series from Mint and Other Records

description: Silver series (some annual but not all) based on mint and other records for Mexico, Guatemala, New Granada, Peru, Potosí & Chile. Assembled by John Jay Tepaske. Mintage from AGI & B.Vicuna Mackenna
DOI: 10.5281/zenodo.2563284
title: Cities At Nights - Community Health

description: Results of the community health analysis of the Cities At Night project (January 2016 - December 2018)
DOI: 10.5281/zenodo.2563285
title: Cities At Nights - Community Health

description: Results of the community health analysis of the Cities At Night project (January 2016 - December 2018)
DOI: 10.7910/dvn/1erqjx
title: EPESE: Established Populations for Epidemiologic Studies of the Elderly, 1981-1993: [East Boston, Massachusetts, Iowa and Washington Counties, Iowa, New Haven, Connecticut, and North Central North Carolina]

description: The goals of the Established Populations for Epidemiologic Studies of the Elderly (EPESE) project were to describe and identify predictors of mortality, hospitalization, and placement in long-term care facilities and to investigate risk factors for chronic diseases and loss of functioning. The survey elicited information from persons 65 years of age and older in four geographic locations: East Boston, Massachusetts, New Haven, Connecticut, Iowa and Washington Counties, Iowa, and five counties in north central North Carolina. The public use baseline data (Part 1) cover demographic characteristics (age, sex, race, income, education, marital status, number of children, employment, and religion), height, weight, social and physical functioning, chronic conditions, related health problems, health habits, self-reported use of dental, hospital, and nursing home services, and depression. Data from six follow-up surveys conducted in all four of the sites are also provided (Parts 2-4 and 6-8), along with information from death certificates for deaths occurring in the first six years of follow-up for all four sites (Part 5).
DOI: 10.7910/dvn/t70prf
title: Replication data for: 'Unexpected Consequences? Bicameral Policymaking Shifts Through Term Limits'

description: Purpose – The imposition of term limits in bicameral (two-chamber) state legislatures could produce unforeseen consequences in the policymaking process. Supporters of term limit rules have not considered that their imposition could fundamentally shift the sequence of policymaking in legislatures. This is important given that research on sequential bicameral policymaking suggests qualities of the lower chamber allow it to cultivate policy expertise such that the upper chamber will defer to the lower chamber in policymaking. This project aims to explore whether this proposed policymaking sequence exists in term-limited states. Design/methodology/approach – A comparison of policy adoptions in states with and without term limits is performed using an original data set on bill adoptions for all US bicameral legislatures that had a regular session between the years 2000 and 2006. Least-squares regression models evaluate whether basic characteristics of legislatures are as relevant as term limit characteristics in explaining the level of outputs from the lower chamber in term-limited states. Findings – In states with term limits, the level of policy adoptions initiated by the lower chamber is lower than levels seen in states without term limits. This finding holds when controlling for other relevant variables that can potentially explain lower chamber productivity. Research limitations/implications – The study analyzes aggregate state-level data and does not interview individual legislators in states with and without term limits on whether term limits can alter future legislative behavior. Originality/value – This study is the first to examine whether the policymaking sequence differs between states that possess and do not possess term limit rules.
DOI: 10.5061/dryad.vk8ms62/2
title: segmentTS

description: Updates to segmentTS will be available in GitHub at
DOI: 10.7910/dvn/yoxpvk
title: Code Coverage and Metrics

description: This dataset contains source code metrics such as lines of code, cyclomatic complexity number, and code coverage data such as statement coverage, branch coverage, path coverage, condition coverage, loop coverage, data coverage and mutation coverage from tools such as Emma, Cobertura, Codecover, JMockit, and Pittest from a number of projects from Github. The code coverage was collected from original test suites present in the programs, and also generated test suites using Randoop.
DOI: 10.17632/dx7sds7ms8.2
title: Data for: The Online Integrated Order Picking and Delivery Considering Pickers’ Learning Effects for An O2O Community Supermarket

description: Research data includes orders’ arrival time and item information in 60 days. The format of data file is mat, generated by Matlab.
DOI: 10.5281/zenodo.2563288
title: Dark Sky Meter - Community Health

description: Results of the community health analysis of the Dark Sky Meter project (January 2016 - December 2018)
DOI: 10.5281/zenodo.2563289
title: Dark Sky Meter - Community Health

description: Results of the community health analysis of the Dark Sky Meter project (January 2016 - December 2018)
DOI: 10.12751/g-node.d315b3
title: The amplitude in periodic neural state trajectories underlies the tempo of rhythmic tapping dataset

description: Data underlying the results published in "The amplitude in periodic neural state trajectories underlies the tempo of rhythmic tapping" by Jorge Gámez, Germán Mendoza, Luis Prado, Abraham Betancourt & Hugo Merchant.
description: IsSupplementTo: The amplitude in periodic neural state trajectories underlies the tempo of rhythmic tapping
DOI: 10.21227/gchd-zx92
title: Locally Linear Embedding and fMRI feature selection in psychiatric classification

description: This dataset collection contains eleven datasets used in Locally Linear Embedding and fMRI feature selection in psychiatric classification.The datasets given in the Links section are reduced subsets of those contained in their respective tar files (a consequence of Mendeley Data's 10GB limitation).The Linked datasets (not the tar files) contain just the MATLAB file and the resting state image (or block-design fMRI for the MRN dataset), where appropriate.The datasets in the tar file contain all of the preprocessing intermediates for the fMRI input to the LLE algorithm.
DOI: 10.7910/dvn/fmphib
title: EI Extended Model and the Fear of Ecological Fallacy, Sociological Methods & Research, Aug 2007; vol. 36: pp. 3 - 25.

description: The growth of literature using EI method has not led to a consensus on the effectiveness of EI as a solution to the ecological inference problem. The most critical scrutiny of EI came from those scholars who directly questioned the model assumptions of EI and the consequences of violations of these assumptions. More recently, the EI’s extended model, rather than its basic model, has been suggested as the best hope to save EI from the trouble of violations of model assumptions, especially logical inconsistency. This paper takes advantage of a unique opportunity to compare the controversial methods, including survey approach, by using aggregate as well as individual level data from an actual election. Furthermore, the true quantities of interest are also available, which guarantees the accuracy of the empirical tests. Our results show that EI basic model provided a better estimate for the black turnout rate, but not for the white turnout, than did the traditional Goodman and double regression methods. However, using an appropriate covariate in the EI extended model can drastically improve the estimation accuracy.