cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/ieda/111288
title: Garnet/melt partition coefficient experiments

description: This dataset presents compiled experimental mineral/melt partitioning data for garnet from the literature (e.g. no unpublished collections). This dataset can help users to calculate differentiation scenarios (by sorting for compositions that match the system of interest), test models or create calibration datasets for models, and facilitate experimental design and data management plans. The format of the data is oriented vertically – each column represents the data from one published experiment – including experimental conditions, source publication, analytical techniques and the composition of the starting composition, liquid, mineral or fluid and the partition coefficient for the elements analyzed. This format is inclusive, and therefore complex, and care should be taken in processing the data from this raw form. Please see the “Readme" tab for further explanations and instructions. This data is presented in the traceDs template, a format for documenting experimental data that is available on the EarthChem website for investigator use. If you find errors in the data transcription or any omissions please contact Roger Nielsen or Gokce Ustunisik (roger.nielsen@sdsmt.edu; gokce.ustunisik@sdsmt.edu) with details of the error or a copy of the paper to be added.
description: Nielsen, R. L., G. Ustunisik, A. B. Weinsteiger, F. J. Tepley III, A. D. Johnston, and A. J. R. Kent (2017), Trace element partitioning between plagioclase and melt: An investigation of the impact of experimental and analytical procedures, Geochem. Geophys. Geosyst., 18 Nielsen, R. L., M. Ghiorso, and T. Trishmann (2015), traceDs: What we have learned about the existing trace element partitioning data during the population phase, Abstract V33C-3119 presented at 2015 Fall Meeting, AGU, San Francisco, Calif.
DOI: 10.1594/ieda/111286
title: Amphibole/melt partition coefficient experiments

description: This dataset presents compiled experimental mineral/melt partitioning data for amphibole from the literature (e.g. no unpublished collections). This dataset can help users to calculate differentiation scenarios (by sorting for compositions that match the system of interest), test models or create calibration datasets for models, and facilitate experimental design and data management plans. The format of the data is oriented vertically – each column represents the data from one published experiment – including experimental conditions, source publication, analytical techniques and the composition of the starting composition, liquid, mineral or fluid and the partition coefficient for the elements analyzed. This format is inclusive, and therefore complex, and care should be taken in processing the data from this raw form. Please see the “Readme" tab for further explanations and instructions. This data is presented in the traceDs template, a format for documenting experimental data that is available on the EarthChem website for investigator use. If you find errors in the data transcription or any omissions please contact Roger Nielsen or Gokce Ustunisik (roger.nielsen@sdsmt.edu; gokce.ustunisik@sdsmt.edu) with details of the error or a copy of the paper to be added.
description: Nielsen, R. L., G. Ustunisik, A. B. Weinsteiger, F. J. Tepley III, A. D. Johnston, and A. J. R. Kent (2017), Trace element partitioning between plagioclase and melt: An investigation of the impact of experimental and analytical procedures, Geochem. Geophys. Geosyst., 18. Nielsen, R. L., M. Ghiorso, and T. Trishmann (2015), traceDs: What we have learned about the existing trace element partitioning data during the population phase, Abstract V33C-3119 presented at 2015 Fall Meeting, AGU, San Francisco, Calif.
DOI: 10.1594/ieda/111283
title: Clinopyroxene/melt partition coefficient experiments

description: This dataset presents compiled experimental mineral/melt partitioning data for clinopyroxene from the literature (e.g. no unpublished collections). This dataset can help users to calculate differentiation scenarios (by sorting for compositions that match the system of interest), test models or create calibration datasets for models, and facilitate experimental design and data management plans. The format of the data is oriented vertically – each column represents the data from one published experiment – including experimental conditions, source publication, analytical techniques and the composition of the starting composition, liquid, mineral or fluid and the partition coefficient for the elements analyzed. This format is inclusive, and therefore complex, and care should be taken in processing the data from this raw form. Please see the “Readme" tab for further explanations and instructions. This data is presented in the traceDs template, a format for documenting experimental data that is available on the EarthChem website for investigator use. If you find errors in the data transcription or any omissions please contact Roger Nielsen or Gokce Ustunisik (roger.nielsen@sdsmt.edu; gokce.ustunisik@sdsmt.edu) with details of the error or a copy of the paper to be added.
description: Nielsen, R.L., Ustunisik, G.U., Weinsteiger, A. W., Kent, A.J., Tepley, F.S., 2017, The trace element diversity of anorthitic MORB plagioclase and their associated melt inclusions, Geochem. Geophys. Geosyst.
DOI: 10.1594/ieda/111285
title: Olivine/melt partition coefficient experiments

description: This dataset presents compiled experimental mineral/melt partitioning data for olivine from the literature (e.g. no unpublished collections). This dataset can help users to calculate differentiation scenarios (by sorting for compositions that match the system of interest), test models or create calibration datasets for models, and facilitate experimental design and data management plans. The format of the data is oriented vertically – each column represents the data from one published experiment – including experimental conditions, source publication, analytical techniques and the composition of the starting composition, liquid, mineral or fluid and the partition coefficient for the elements analyzed. This format is inclusive, and therefore complex, and care should be taken in processing the data from this raw form. Please see the “Readme" tab for further explanations and instructions. This data is presented in the traceDs template, a format for documenting experimental data that is available on the EarthChem website for investigator use. If you find errors in the data transcription or any omissions please contact Roger Nielsen or Gokce Ustunisik (roger.nielsen@sdsmt.edu; gokce.ustunisik@sdsmt.edu) with details of the error or a copy of the paper to be added.
description: Nielsen, R. L., M. Ghiorso, and T. Trishmann (2015), traceDs: What we have learned about the existing trace element partitioning data during the population phase, Abstract V33C-3119 presented at 2015 Fall Meeting, AGU, San Francisco, Calif.
DOI: 10.1594/ieda/111237
title: Sediment geochemical and geochronological analyses of OC170-26-159, Pacific-Antarctic Ridge

description: This dataset encompasses several different measurements on core OC170-26-159, including: 1) planktonic foraminiferal oxygen isotopes (0-230 kyr BP) and benthic oxygen isotopes (~120-150 kyr BP) measured on a Finnigan MAT 253 at the University of Michigan and Georgia Tech, 2) bulk elemental concentrations (0-230 kyr BP) measured on Thermo Element 2 at UCONN, 3) basaltic glass shard major elements (in two ash layers centered at ~140 kyr BP and 230 kyr BP) measured at Caltech using an electron microprobe, 4) trace element composition of the same shards determined using laser ablation ICP-MS at Caltech, 5) volatile content of the glass shards determined using FTIR at Caltech, and 6) shard grain size (for each ash layer) and settling velocity data for three separate size fractions of ash shards determined at UCONN. The full details of each method are described in the G-cubed related publication.
description: Lund, D. C., Seeley, E. I., Asimow, P. D., Lewis, M. J., McCart, S. E., & Mudahy, A. A. (2018). Anomalous Pacific-Antarctic ridge volcanism precedes Glacial Termination 2. Geochemistry, Geophysics, Geosystems, 19.
DOI: 10.1594/ieda/111268
title: Detrital zircon geochronological dataset of Zhu 2 depression, Pearl River Mouth Basin, South China Sea

description: We conducted detrital zircon U-Pb dating through laser ablation-inductively coupled plasma mass spectrometry (LA-ICPMS) at the State Key Laboratory of Geological Processes and Mineral Resources. The new detrital zircon U-Pb ages from Paleogene formations in seven boreholes, southern Pearl River Mouth Basin are used to investigate local versus regional influences on provenance.
description: Wang, Wei; Yang, Xianghua; Bidgoli, Tandis; Ye, Jiaren. Detrital zircon geochronology reveals source-to-sink relationships in the Pearl River Mouth Basin, China. Sedimentary Geology. In Review.
DOI: 10.1594/ieda/111291
title: Molybdenum Isotopes of the Subduction-related Orogenic Potassic Magmas of Central-Southern Italy

description: The potassic and ultrapotassic magmas of the Tuscan Magmatic Province and Mt. Vesuvius represent two well characterised subduction-related magmatic associations along the Tyrrhenian border of the Italian peninsula. They display exotic and distinctive geochemical and radiogenic isotope features, which were traditionally related to differences in the lithology of the subducted material in their respective mantle sources. Their Mo content, when correlated to an other trace element with similar degree of incompatibility such as Ce, displays significant differences in terms of Ce/Mo values (ca. 25 for Vesuvius and ca. 340 for Tuscan magmas). However, the two magmatic suites show surprisingly similar δ98/95Mo values (0.10 - 0.26 ‰ for Vesuvius and 0.07 – 0.22 ‰ for Tuscan Magmatic Province), which are significantly heavier than typical mid-ocean ridge basalts. While the δ98/95Mo values implicate an isotopically heavy sedimentary component recycled into their respective mantle sources, the different Ce/Mo ratios reflect contrasting elemental fractionation during sediment melting related to the lithology and consequent residual mineralogy of the subducted sedimentary material undergoing melting. This dataset presents Mo, δ98/95Mo, and trace element analysis measured by ICP-MS and Sr and Nd ratios measured by TIMS in orogenic potassic magmas and sedimentary end-members from Central-Southern Italy.
description: Casalini M., Avanzinelli R., Elliott T., Tommasini S., Conticelli S., "Ce/Mo and Molybdenum Isotope Systematics in Subduction-related Orogenic Potassic Magmas of Central-Southern Italy." Geochemistry, Geophysics, Geosystems.
DOI: 10.1594/ieda/111290
title: Silicate mineral compositions from a granulite facies mafic dike, northern Madison Range, Montana

description: These data are mineral compositions measured by electron microprobe, presented in the 2012 publication in Earth and Planetary Science Letters by Ault et al. The data are from one sample of a metamorphosed mafic dike sample (M08-72). The sample was targeted to help constrain conditions and timing of metamorphism and deformation in the Bear Trap Canyon area of the northern Madison Range, southwestern Montana. Pressure and temperature (P-T) equilibrium conditions calculated for the sample mineral assemblage constrain representative metamorphic conditions. Zircon geochronology data for this sample is also presented in the EPSL publication.
description: Alexis K. Ault, Rebacca M. Flowers, Kevin H. Mahan, (2012), "Silicate mineral compositions from a granulite facies mafic dike, northern Madison Range, Montana." Earth and Planetary Science Letters, (339-340): 57-66
DOI: 10.1594/ieda/111282
title: Major and trace element data and Sr-Nd-Pb-Hf isotope ratios for Bermuda volcanic rocks

description: The volcanic edifice of Bermuda is composed of two interbedded lithologies: a silica undersaturated alkaline suite and a silica saturated suite. This dataset contains the major element (collected via XRF) and trace element (collected via LA-ICP-MS) analysis for both the silica undersaturated and silica saturated units. Age of the alkaline suite is ~30.9 Ma while the silica saturate suite has not been successfully dated. The Pb-Sr-Nd-Hf radiogenic isotopic data (collected via MC-ICP-MS) was only collected for a subset of the silica undersaturated alkaline and the silica saturated suites.
description: Mazza et al. (under revision) "Sampling the Volatile Rich Transition Zone beneath Bermuda". Nature.
DOI: 10.1594/ieda/111284
title: Plagioclase/melt partition coefficient experiments

description: This dataset presents compiled experimental mineral/melt partitioning data for plagioclase from the literature (e.g. no unpublished collections). This dataset can help users to calculate differentiation scenarios (by sorting for compositions that match the system of interest), test models or create calibration datasets for models, and facilitate experimental design and data management plans. The format of the data is oriented vertically – each column represents the data from one published experiment – including experimental conditions, source publication, analytical techniques and the composition of the starting composition, liquid, mineral or fluid and the partition coefficient for the elements analyzed.  This format is inclusive, and therefore complex, and care should be taken in processing the data from this raw form. Please see the “Readme" tab for further explanations and instructions. This data is presented in the traceDs template, a format for documenting experimental data that is available on the EarthChem website for investigator use. If you find errors in the data transcription or any omissions please contact Roger Nielsen or Gokce Ustunisik (roger.nielsen@sdsmt.edu; gokce.ustunisik@sdsmt.edu) with details of the error or a copy of the paper to be added.
description: Nielsen, R. L., G. Ustunisik, A. B. Weinsteiger, F. J. Tepley III, A. D. Johnston, and A. J. R. Kent (2017), Trace element partitioning between plagioclase and melt: An investigation of the impact of experimental and analytical procedures, Geochem. Geophys. Geosyst., 18
DOI: 10.1594/ieda/111280
title: Geochemistry and grain size for sediment core JPC14 from Golfo Elefantes, Chilean Patagonia

description: This dataset contains 1) inorganic geochemical data obtained using an Itrax XRF core scanner, 2) inorganic geochemical concentrations measured by ICP-AES on a series of 44 subsamples, and 3) grain-size data for 92 size classes measured by laser diffraction particle size analysis. Sediment core JPC14 was obtained from Golfo Elefantes during cruise NPB05-05 in June-July 2005.
description: Bertrand, S., Hughen, K. A., Lamy, F., Stuut, J. B. W., Torrejón, F., & Lange, C. B. (2012). Precipitation as the main driver of Neoglacial fluctuations of Gualas glacier, Northern Patagonian Icefield. Climate of the Past, 8(2), 519–534.

Bertrand, S., Hughen, K., & Giosan, L. (2015). Limited influence of sediment grain size on elemental XRF core scanner measurements. In I. W. Croudace & R. G. Rothwell (Eds.), Micro-XRF Studies of Sediment Cores: Applications of a non-destructive tool for the environmental sciences (pp. 473–490). Dordrecht: Springer Netherlands. https://doi.org/10.1007/978-94-017-9849-5_19

Bertrand, S., Hughen, K. A., Sepúlveda, J., & Pantoja, S. (2012b). Geochemistry of surface sediments from the fjords of Northern Chilean Patagonia (44-47°S): Spatial variability and implications for paleoclimate reconstructions. Geochimica et Cosmochimica Acta, 76, 125–146. https://doi.org/10.1016/j.gca.2011.10.028

Liu, D., Bertrand, S., Gert Jan, Weltje. (submitted). An empirical method to predict sediment grain size from inorganic geochemical measurements. Geochemistry, Geophysics, Geosystems.
DOI: 10.1594/ieda/111279
title: Geochemistry and grain size for sediment core PC29A from Quitralco Fjord, Chilean Patagonia

description: This dataset contains 1) inorganic geochemical data obtained using an Itrax XRF core scanner, 2) inorganic geochemical concentrations measured by ICP-AES on a series of 102 subsamples, and 3) grain-size data for 92 size classes measured by laser diffraction particle size analysis. Sediment core PC29A was obtained from Quitralco Fjord during cruise CIMAR (Cruceros de Investigacion Marina) Fiordos 7 in February 2001.
description: Bertrand, S., Hughen, K., Sepúlveda, J., & Pantoja, S. (2014). Late Holocene covariability of the southern westerlies and sea surface temperature in northern Chilean Patagonia. Quaternary Science Reviews, 105, 195–208.

Bertrand, S., Hughen, K., & Giosan, L. (2015). Limited influence of sediment grain size on elemental XRF core scanner measurements. In I. W. Croudace & R. G. Rothwell (Eds.), Micro-XRF Studies of Sediment Cores: Applications of a non-destructive tool for the environmental sciences (pp. 473–490). Dordrecht: Springer Netherlands. https://doi.org/10.1007/978-94-017-9849-5_19

Bertrand, S., Hughen, K. A., Sepúlveda, J., & Pantoja, S. (2012b). Geochemistry of surface sediments from the fjords of Northern Chilean Patagonia (44-47°S): Spatial variability and implications for paleoclimate reconstructions. Geochimica et Cosmochimica Acta, 76, 125–146. https://doi.org/10.1016/j.gca.2011.10.028

Liu, D., Bertrand, S., Gert Jan, Weltje. (submitted). An empirical method to predict sediment grain size from inorganic geochemical measurements. Geochemistry, Geophysics, Geosystems.
DOI: 10.1594/ieda/111277
title: Glacier Creek Preserve Prairie Weather Data 2018

description: Hourly meteorological and soil data for 2018 on a restored prairie ridgetop at the University of Nebraska's Glacier Creek Preserve in Bennington, NE. The Campbell Scientific meteorological station is powered by a solar panel (SP10) and rechargeable battery (CH150). Data is collected with a datalogger (CR1000) housed in a fiberglass enclosure and includes the following sensors: anemometer (R.M. Young’s 03002 Wind Sentry Set), all season pyranometer (SP230), precipitation sensor (Texas Electronics Tipping Bucket Rain Gages), temperature and relative humidity sensor (HC2S3), barometer (CS106), soil moisture, temperature and electrical conductivity at four depths (CS655), and high-resolution digital network cameras (CC5MPX). Evapotranspiration is calculated daily.
DOI: 10.1594/ieda/111278
title: Glacier Creek Preserve Agriculture Weather Data 2018

description: Hourly meteorological and soil data for 2018 on an agricultural ridgetop (soybean crop) at the University of Nebraska's Glacier Creek Preserve in Bennington, NE. The Campbell Scientific meteorological station is powered by a solar panel (SP10) and rechargeable battery (CH150). Data is collected with a datalogger (CR1000) housed in a fiberglass enclosure and includes the following sensors: anemometer (R.M. Young’s 03002 Wind Sentry Set), all season pyranometer (SP230), precipitation sensor (Texas Electronics Tipping Bucket Rain Gages), temperature and relative humidity sensor (HC2S3), barometer (CS106), soil moisture, temperature and electrical conductivity at four depths (CS655), and high-resolution digital network cameras (CC5MPX). Evapotranspiration is calculated daily.
DOI: 10.1594/ieda/111272
title: Silicate mineral compositions for metamorphic schist and amphibolite, northern Madison Range, southwestern Montana

description: These data are mineral compositions measured by electron microprobe, presented in the 2015 publication in Lithosphere by Condit et al. Two samples of Bear Basin schist (GP7c and GP7f) and one mafic dike sample (AA09-61) were targeted to help constrain conditions and timing of metamorphism and deformation in the Gallatin Peak terrane of the northern Madison Range, southwestern Montana. The Bear Basin schist was sampled in a pelitic horizon because the mineral assemblages are amenable to quantitative thermobarometry and monazite geochronology. The mafic dikes were targeted because they represent the youngest metamorphosed and deformed intrusive units in the study area. Pressure and temperature (P-T) equilibrium conditions calculated from all three samples constrain representative metamorphic conditions in the northwest portion of the Gallatin Peak terrane. Geochronology data for these samples is also presented in the Lithosphere publication.
description: Cailey B. Condit, Kevin H. Mahan, Alexis K. Ault, and Rebecca M. Flowers, (2015), "Foreland-directed propagation of high-grade tectonism in the deep roots of a Paleoproterozoic collisional orogen, SW Montana, USA." Lithosphere, 7(6): 625-645.
DOI: 10.1594/ieda/111274
title: Major and minor element data and mineralogical composition of products from kinetic dolomitization laboratory experiments

description: This dataset presents ICP-OES major and minor element data and XRD mineralogical compositions of reaction products from laboratory experiments focused on kinetics of dolomitization of calcite in saline fluids at 200ºC.
description: Vandeginste, V., Snell, O., Hall, M.R., Steer, E., Vandeginste, A., (2019) "Acceleration of dolomitization by zinc in saline waters". Under review with Nature Communications
DOI: 10.1594/ieda/111271
title: Carbon and noble gas data from Costa Rica seeps

description: Noble gas and carbon data were measured in cold seeps in Costa Rica in order to understand the sources of forearc fluids and processes acting to modify the geochemical signals. 2017 noble gases were measured on the Thermo SFT/Argus system at the University of Oxford. Helium and carbon was also measured at Scripps Institution of Oceanography (on pre 2017 samples) using MAP 215 and Thermo-Finnigan Delta XPPlus. The 2017 DIC measurements were done at the Earth-Life Science Institute, Tokyo Institute for Technology using an Agilent 6890N gas chromatograph attached to a Thermo-Finnigan Delta XPPlus.
description: Barry, P. H., et al. (2019). Forearc carbon sink reduces long-term volatile recycling into the mantle. Nature, 568(7753), 487.
DOI: 10.1594/ieda/111269
title: Sr and Nd analyses of Congo sediments and Kalahari duricrusts

description: We investigated red-beds, boulders of silcretes and calcretes exposed around the margins and in river systems of the Congo Basin. We analyzed trace elements, 87Sr/86Sr and 143Nd/144Nd of 21 samples, and performed dilute leaching experiments on 3 of these samples to determine the source provenance and potential to release Sr during weathering. These samples were analyzed by ICP-MS at the University of Cape Town (UCT) and Nelson Mandela University (NMU) in South Africa.
description: Linol, Bastien; de Villiers, Stephanie; de Wit, Maarten, (2019), "Accelerated contribution of the paleo-Congo River to global seawater 87Sr/86Sr change following Eocene-Oligocene collapse of the African Surface." Gcubed, submitted.
DOI: 10.1594/ieda/111270
title: Characterization of plagioclase-hosted melt inclusions in A91-1R (Blanco Transform Fault)

description: We present a database characterizing the composition and volatile contents of plagioclase-hosted melt inclusions from a unique sample from the Blanco Transform Fault (A91-1R). The melt inclusions were homogenized on a 1-atm vertical furnace at two temperatures from 30 min to 4 days to gain a better understanding of the post entrapment processes induced by the homogenization experiments. The composition and volatile contents of the melt inclusions indicate their mantle origins.
description: Drignon, Melissa J.; Nielsen, Roger L.; Tepley, Frank J. III; Bodnar, Robert J., (2018), "Upper Mantle Origin of Plagioclase Megacrysts from Plagioclase Ultraphyric MORB". Geology, 47(1): 43-46.

Drignon, Melissa J.; Nielsen, Roger L.; Tepley, Frank J. III; Bodnar, Robert J., (2019), "Reequilibration processes occurring in plagioclase-hosted melt inclusions from plagioclase ultraphyric basalts", Geochemistry, Geophysics, Geosystems, 10.1029/2018GC007795.