cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/ieda/111156
title: Jemez River Basin Soil Solution Chemistry 2011 (New Mexico, USA)

description: **This is a new version of a previously submitted dataset.** Soil solution samples in the Jemez River Basin field sites of the Catalina-Jemez Critical Zone Observatory (CZO) are collected with two types of soil solution samples: i) Prenart Super Quartz suction cups (www.prenart.dk). Prenart suction cups are optimized for all chemistry analyses and were installed without addition of Si-slurry to allow for artifact-free Si analyses. Applied suction for each Prenart is ~ 60kPa. ii) Custom made, fiberglass wick-based passive capillary wick samplers (PCaps, Perdrial et al. 2012). PCaps are optimized for water flux determination and sampling for organic carbon, most anions and metals. PCap samples should however not be used for major cations (Na, Mg, Si, K, Ca) and dissolved inorganic carbon because of artifacts from the fiberglass materials (see Perdrial et al (2014) for a complete list). Passive suction, based on the length of the hanging water column, is ~3 kPa. Soil solution samplers were installed in each of six pits in the Mixed Conifer Zero Order Basin (MC-ZOB) at 3 (PCaps) and 4 (Prenarts) depths. Pit locations were selected to capture differences in catchment aspect (SE facing: Pit 3 and 4, NW facing: Pit 1 and 6), landscape position (hollow Pit 2 and 5, planar Pit 1 and 6, divergent Pit 3, convergent Pit 4). All samplers are collocated with Decagon soil moisture and temperature probes.
description: Perdrial, J.N., Perdrial, N., Harpold, A., Gao, X., LaSharr, K.M., Chorover, J. (2012) Impacts of sampling dissolved organic matter with passive capillary wicks versus aqueous soil extraction. Soil Science Society of America Journal, 76: 2019-2030, doi: 10.2136/sssaj2012.0061. Vazquez-Ortega, A., Perdrial, J., Harpold, A., Zapata-Rios, X., Rasmussen, C., McIntosh, J., Schaap, M., Pelletier, J. D., Brooks, P. D., Amistadi, M. K., and Chorover, J. (2015) Rare earth elements as reactive tracers of biogeochemical weathering in forested rhyolitic terrain. Chemical Geology, 391: 19-32, doi: 10.1016/j.chemgeo.2014.10.016. Perdrial, J. N., Perdrial, N., Vazquez-Ortega, A., Porter, C., Leedy, J., and Chorover, J. (2014) Experimental Assessment of Passive Capillary Wick Sampler Suitability for Inorganic Soil Solution Constituents. Soil Science Society of America Journal, 78(2): 486-495, doi: 10.2136/sssaj2013.07.0279. Vazquez-Ortega, A., Huckle, D., Perdrial, J., Amistadi, M. K., Durcik, M., Rasmussen, C., McIntosh, J., Chorover, J. (2016) Solid-phase redistribution of rare earth elements in hillslope pedons subjected to different hydrologic fluxes. Chemical Geology, 426: 1-18, doi: 10.1016/j.chemgeo.2016.01.001.
DOI: 10.1594/ieda/111155
title: Jemez River Basin Soil Solution Chemistry 2012 (New Mexico, USA)

description: Soil solution samples in the Jemez River Basin field sites of the Catalina-Jemez Critical Zone Observatory (CZO) are collected with two types of soil solution samples: i) Prenart Super Quartz suction cups (www.prenart.dk). Prenart suction cups are optimized for all chemistry analyses and were installed without addition of Si-slurry to allow for artifact-free Si analyses. Applied suction for each Prenart is ~ 60kPa. ii) Custom made, fiberglass wick-based passive capillary wick samplers (PCaps, Perdrial et al. 2012). PCaps are optimized for water flux determination and sampling for organic carbon, most anions and metals. PCap samples should however not be used for major cations (Na, Mg, Si, K, Ca) and dissolved inorganic carbon because of artifacts from the fiberglass materials (see Perdrial et al (2014) for a complete list). Passive suction, based on the length of the hanging water column, is ~3 kPa. Soil solution samplers were installed in each of six pedons in the Mixed Conifer Zero Order Basin (MC-ZOB) and the fire impacted site (2011 Burned ZOB) at 3 (PCaps) and 4 (Prenarts) depths, respectively. Pedon locations were selected to capture differences in catchment aspect (MC-ZOB SE facing: Pit 3 and 4, NW facing: Pit 1 and 6), landscape position (MC-ZOB: hollow Pit 2 and 5, planar Pit 1 and 6, divergent Pit 3, convergent Pit 4), elevation and burn severity (co-varying in 2011 Burned ZOB: low Pit 1 and 2, mid Pit 3, high Pit 4 to 6). All samplers are collocated with Decagon soil moisture and temperature probes.
description: Perdrial, J.N., Perdrial, N., Harpold, A., Gao, X., LaSharr, K.M., Chorover, J. (2012) Impacts of sampling dissolved organic matter with passive capillary wicks versus aqueous soil extraction. Soil Science Society of America Journal, 76: 2019-2030, doi: 10.2136/sssaj2012.0061.

Vazquez-Ortega, A., Perdrial, J., Harpold, A., Zapata-Rios, X., Rasmussen, C., McIntosh, J., Schaap, M., Pelletier, J. D., Brooks, P. D., Amistadi, M. K., and Chorover, J. (2015) Rare earth elements as reactive tracers of biogeochemical weathering in forested rhyolitic terrain. Chemical Geology, 391: 19-32, doi: 10.1016/j.chemgeo.2014.10.016.

Perdrial, J. N., Perdrial, N., Vazquez-Ortega, A., Porter, C., Leedy, J., and Chorover, J. (2014) Experimental Assessment of Passive Capillary Wick Sampler Suitability for Inorganic Soil Solution Constituents. Soil Science Society of America Journal, 78(2): 486-495, doi: 10.2136/sssaj2013.07.0279.

Vazquez-Ortega, A., Huckle, D., Perdrial, J., Amistadi, M. K., Durcik, M., Rasmussen, C., McIntosh, J., Chorover, J. (2016) Solid-phase redistribution of rare earth elements in hillslope pedons subjected to different hydrologic fluxes. Chemical Geology, 426: 1-18, doi: 10.1016/j.chemgeo.2016.01.001.
DOI: 10.1594/ieda/111152
title: Noble Gas and Helium Isotope Measurements of Seawater from the Amundsen Sea (Antarctica)

description: This dataset contains noble gas and helium isotope measurements of seawater samples collected in the vicinity of the Amundsen Sea, along the coast of Antarctica during the Ocean2ice cruise aboard the RRS James Clark Ross in the 2013/2014 Antarctic Summer.
DOI: 10.1594/ieda/111149
title: XRF Analyses of Sediment Cores from the Japan Margin Trench

description: The samples were collected from the R/V Natsushima 13-02 and 13-19 from the Japan Trench slope and Mid-Slope terrace for studying earthquake generated turbidites. The focus was on the 2011 Mw9.0 Tohoku earthquake and tsunami. Wet chemistry x-ray fluorescence elemental analyses were conducted with a Spectro XEPOS III® X-Ray Fluorescence Spectrometer with a Palladium X-Ray tube and silicon drift detector (SDD) in the laboratory of Dr. Bopp at Rensselaer Polytechnic Institute. The samples were packed in 3.2cm diameter polyethylene cylinders with one end covered by a 4μ prolene® (polypropylene) film. The samples were irradiated through the prolene with emissions from three secondary targets (Mo; Al2O3 (barkla scatter); and HOPG (Bragg interference)). Quantification was based on a proprietary program, TurboQuant Powders, supplied with the instrument calibrated to analyses of sediment and soil Standard Reference Materials (NIST SRMs 1944, 2702, 2704, and 2709).  Additional assessment of the data quality was provided by XRF analyses of internal laboratory standards and other sediment samples that had been previously analyzed by ICP/MS or atomic absorption spectroscopy in the research groups of one of Richard Bopp at RPI and the Lamont-Doherty Geological Observatory (LDEO) of Columbia University.  For the elements reported (Cu, Pb, Zn, Cr, Ni, As, Si, Al, Fe, Mn, Ti, Ca, Sr, and K) the relative standard deviation of multiple analyses of SRMs and samples was 5% or less.  Applications of this XRF technique to sediment sample analysis have been described in several publications from the laboratory at RPI (Blount, 2009; Merrill, 2010; Graber et al., 2010).
description: McHugh, C.M., Kanamatsu, T., Seeber, L., Bopp, R., Cormier, M.-H., Usami, K., 2016. Remobilization of surficial slope sediment triggered by the A.D. 2011 Mw9 Tohoku-Oki earthquake and tsunami along the Japan Trench. Geology 44(5), 391-394
DOI: 10.1594/ieda/111153
title: Radioisotopic Analyses of Sediment Cores from the Japan Margin Trench

description: The samples were collected from the R/V Natsushima 13-02 and 13-19 from the Japan Trench slope and Mid-Slope terrace for studying earthquake genereated turbidites. The focus was on the 2011 Mw9.0 Tohoku earthquake and tsunami. Radionuclide measurements were carried out using a gamma counter with a germanium detector operated in the “well” configuration (ORTEC GWL-120) at the laboratory of Dr. Bopp at Rensselaer Polytechnic Institute.  Blank corrections were applied to each sample based on the analysis of empty sample containers.  Background corrections were applied to each radionuclide based on the sample count rate at energies just above and just below each peak of interest.  Detector efficiency was calibrated using an NBS sediment standard (River sediment NBS 4350B), a liquid NBS standard (NBS 4953-C) that was used to prepare spiked sediments (G-standards), and secondary standards (D-standards) prepared at LDEO and calibrated to NBS standards. Certified reference material supplied by the National Institute of Metrology, Beijing, China (River sediment GBW08304a) and a secondary standard (LGP) analyzed for 210Pb(tot) by alpha spectrometry at the LDEO were also used as standards. The samples were analyzed for 137Cs, 7Be, 234Th, and excess 210Pb using procedures by Bopp et al. (2006).
description: McHugh, C.M., Kanamatsu, T., Seeber, L., Bopp, R., Cormier, M.-H., Usami, K. (2016) Remobilization of surficial slope sediment triggered by the A.D. 2011 Mw9 Tohoku-Oki earthquake and tsunami along the Japan Trench. Geology, 44(5), 391-394.
DOI: 10.1594/ieda/111145
title: Santa Catalina Mountains Soil Solution Chemistry 2014 (Arizona, USA)

description: Soil solution samples in the Santa-Catalina Mountain field sites of the Catalina-Jemez Critical Zone Observatory (CZO) are collected with three types of soil solution samples: i) Prenart Super Quartz suction cups (www.prenart.dk) and ii) SoilMoisture suction cups (SoilMoisture Equipment Corp., Santa Barbara, CA) and iii) custom made zero-tension sampler (Hinckley et al., 2008). Prenart suction cups are optimized for all chemistry analyses and were installed without addition of Si-slurry to allow for artifact-free Si analyses. Applied suction for each Prenart is ~ 50kPa and SoilMoisture suction cups are sampled with a suction of 70-80kpa. Both suction cup types are optimized for all chemistry analyses with the exception of dissolved organic matter in the case of the SoilMoisture ones (due to potential sorption of DOM on the porous ceramic material). Zero-tension samplers are optimized for water flux determination at saturated flow and sampling for various chemistry analyses. In Marshall Gulch there are 8 SoilMoisture suction cups in the schist site and 7 in the granite site in both convergent and divergent landscape positions. These soil solution samplers are co-located with piezometers measuring water table depth within the soil profile. In the Oracle Ridge site there are 8 pits each equipped with 2 Prenarts and 1 SoilMoisture ceramic cup lysimeter. These samplers are co-located with Decagon Em5b data loggers with EC-5 soil moisture sensors and ECT soil temperature sensors. The B2 Desert site Schist and a Granite sites are both equipped with 7 zero-tension samplers (Hinckley et al., 2008) in both divergent and convergent landscape positions as well one SoilMoisture ceramic cup lysimeter. These samplers are co-located with Decagon Em5b data loggers with EC-5 soil moisture sensors and ECT soil temperature sensors.
description: Trostle, K.D., Runyon, J.R., Pohlmann, M.A., Redfield, S.E., Pelletier, J., McIntosh, J., and Chorover, J. (2016) Colloids and Organic Matter Complexation Control Trace Metal Concentration-Discharge Relationships in Marshall Gulch Stream. Water Resources Research, 52(10): 7931–7944, doi: 10.1002/2016WR019072.
DOI: 10.1594/ieda/111144
title: Jemez River Basin Soil Solution Chemistry 2014 (New Mexico, USA)

description: Soil solution samples in the Jemez River Basin field sites of the Catalina-Jemez Critical Zone Observatory (CZO) are collected with the following two types of soil solution samplers: i) Prenart Super Quartz suction cups (www.prenart.dk). Prenart suction cups are optimized for all chemistry analyses and were installed without addition of Si-slurry to allow for artifact-free Si analyses. Applied suction for each Prenart is ~ 60 kPa. ii) Custom made, fiberglass wick-based passive capillary wick samplers (PCaps, Perdrial et al. 2012). PCaps are optimized for water flux determination and sampling for organic carbon, most (non-carbonate) anions and trace metals. PCap samples should however not be used for major cations (Na, Mg, Si, K, Ca) and dissolved inorganic carbon because of artifacts from the fiberglass materials (see Perdrial et al (2014) for a complete list). Passive (continuous) suction, based on the length of the hanging water column, is ~3 kPa. Soil solution samplers were installed in each of six pedons in the Mixed Conifer Zero Order Basin (MC-ZOB) and the fire impacted site (2011 Burned ZOB) at 3 (PCaps) and 4 (Prenarts) depths, respectively. Pedon locations were selected to capture differences in catchment aspect (MC-ZOB SE facing: Pit 3 and 4, NW facing: Pit 1 and 6), landscape position (MC-ZOB: hollow Pit 2 and 5, planar Pit 1 and 6, divergent Pit 3, convergent Pit 4), elevation and burn severity (co-varying in 2011 Burned ZOB: low Pit 1 and 2, mid Pit 3, high Pit 4 to 6). All samplers are co-located with Decagon soil moisture and temperature probes. MC-ZOB was subject to a high intensity wildfire (Thompson Ridge fire) in June 2013 and was then renamed to 2013 Burned ZOB.
description: Perdrial, J.N., Perdrial, N., Harpold, A., Gao, X., LaSharr, K.M., Chorover, J. (2012) Impacts of sampling dissolved organic matter with passive capillary wicks versus aqueous soil extraction. Soil Science Society of America Journal, 76: 2019-2030, doi: 10.2136/sssaj2012.0061.

Vazquez-Ortega, A., Perdrial, J., Harpold, A., Zapata-Rios, X., Rasmussen, C., McIntosh, J., Schaap, M., Pelletier, J. D., Brooks, P. D., Amistadi, M. K., and Chorover, J. (2015) Rare earth elements as reactive tracers of biogeochemical weathering in forested rhyolitic terrain. Chemical Geology, 391: 19-32, doi: 10.1016/j.chemgeo.2014.10.016.

Perdrial, J. N., Perdrial, N., Vazquez-Ortega, A., Porter, C., Leedy, J., and Chorover, J. (2014) Experimental Assessment of Passive Capillary Wick Sampler Suitability for Inorganic Soil Solution Constituents. Soil Science Society of America Journal, 78(2): 486-495, doi: 10.2136/sssaj2013.07.0279.

Vazquez-Ortega, A., Huckle, D., Perdrial, J., Amistadi, M. K., Durcik, M., Rasmussen, C., McIntosh, J., Chorover, J. (2016) Solid-phase redistribution of rare earth elements in hillslope pedons subjected to different hydrologic fluxes. Chemical Geology, 426: 1-18, doi: 10.1016/j.chemgeo.2016.01.001.
DOI: 10.1594/ieda/111143
title: Jemez River Basin Soil Solution Chemistry 2013 (New Mexico, USA)

description: Soil solution samples in the Jemez River Basin field sites of the Catalina-Jemez Critical Zone Observatory (CZO) are collected with two types of soil solution samples: i) Prenart Super Quartz suction cups (www.prenart.dk). Prenart suction cups are optimized for all chemistry analyses and were installed without addition of Si-slurry to allow for artifact-free Si analyses. Applied suction for each Prenart is ~ 60kPa. ii) Custom made, fiberglass wick-based passive capillary wick samplers (PCaps, Perdrial et al. 2012). PCaps are optimized for water flux determination and sampling for organic carbon, most anions and metals. PCap samples should however not be used for major cations (Na, Mg, Si, K, Ca) and dissolved inorganic carbon because of artifacts from the fiberglass materials (see Perdrial et al (2014) for a complete list). Passive suction, based on the length of the hanging water column, is ~3 kPa. Soil solution samplers were installed in each of six pedons in the Mixed Conifer Zero Order Basin (MC-ZOB) and the fire impacted site (2011 Burned ZOB) at 3 (PCaps) and 4 (Prenarts) depths, respectively. Pedon locations were selected to capture differences in catchment aspect (MC-ZOB SE facing: Pit 3 and 4, NW facing: Pit 1 and 6), landscape position (MC-ZOB: hollow Pit 2 and 5, planar Pit 1 and 6, divergent Pit 3, convergent Pit 4), elevation and burn severity (co-varying in 2011 Burned ZOB: low Pit 1 and 2, mid Pit 3, high Pit 4 to 6). All samplers are co-located with Decagon soil moisture and temperature probes. MC-ZOB was subject to a high intensity wildfire (Thompson Ridge fire) in June 2013 and was then renamed to 2013 Burned ZOB.
description: Perdrial, J.N., Perdrial, N., Harpold, A., Gao, X., LaSharr, K.M., Chorover, J. (2012) Impacts of sampling dissolved organic matter with passive capillary wicks versus aqueous soil extraction. Soil Science Society of America Journal, 76: 2019-2030, doi: 10.2136/sssaj2012.0061.

Vazquez-Ortega, A., Perdrial, J., Harpold, A., Zapata-Rios, X., Rasmussen, C., McIntosh, J., Schaap, M., Pelletier, J. D., Brooks, P. D., Amistadi, M. K., and Chorover, J. (2015) Rare earth elements as reactive tracers of biogeochemical weathering in forested rhyolitic terrain. Chemical Geology, 391: 19-32, doi: 10.1016/j.chemgeo.2014.10.016.

Perdrial, J. N., Perdrial, N., Vazquez-Ortega, A., Porter, C., Leedy, J., and Chorover, J. (2014) Experimental Assessment of Passive Capillary Wick Sampler Suitability for Inorganic Soil Solution Constituents. Soil Science Society of America Journal, 78(2): 486-495, doi: 10.2136/sssaj2013.07.0279.

Vazquez-Ortega, A., Huckle, D., Perdrial, J., Amistadi, M. K., Durcik, M., Rasmussen, C., McIntosh, J., Chorover, J. (2016) Solid-phase redistribution of rare earth elements in hillslope pedons subjected to different hydrologic fluxes. Chemical Geology, 426: 1-18, doi: 10.1016/j.chemgeo.2016.01.001.
DOI: 10.1594/ieda/111138
title: Whole Rock Composition Data for Garnet Pyroxenites from Arizona

description: Whole rock composition data for garnet pyroxenites from Arizona.
DOI: 10.1594/ieda/110998
title: Electron microprobe analyses of spinel group minerals and ilmenite in Apollo 15 rake samples of igneous origin

description: This dataset contains quantitative electron microprobe analyses of spinel group minerals and ilmenites in 33 rocks of igneous origin from the Apollo 15 rake samples
description: C.E. Nehru, Martin Prinz, Eric Dowty, Klaus Keil, (1973) "Electron microprobe analyses of spinel group minerals and ilmenite in Apollo 15 rake samples of igneous origin", Department of Geology & Institute of Meteoritics, University of New Mexico, Special publication 10
DOI: 10.1594/ieda/111107
title: Electron Microprobe Analyses of Spinel, Fe-Ti Oxides and Metal from Apollo 17 Rake Sample Mare Basalts

description: This dataset contains quantitative electron microprobe analyses of spinel, armalcolite, ilmenite, rutile, metal, tranquillityite and zirconolite in 29 Apollo 17 mare basalts.
description: Warner, Richard D., Berkley, John L., Mansker, William L., Warren, Richard G., Keil, Klaus (1976) Electron Microprobe Analyses of Spinel, Fe-Ti Oxides and Metal from Apollo 17 Rake Sample Mare Basalts, Department of Geology & Institute of Meteoritics, University of New Mexico, Special publication 16
DOI: 10.1594/ieda/100746
title: Detrital zircon U-Pb geochronology data from the Potsdam Group

description: This geochronology dataset contains U-Pb isotopic ratios and radiometric ages from detrital zircon grains that complement GSA Bulletin submission, B31749R1, entitled "Early Paleozoic rifting and reactivation of a passive-margin rift: insights from detrital zircon provenance signatures of the Potsdam Group, Ottawa graben". The detrital zircons are from the Cambrian to Ordovician Potsdam Group, and samples were obtained in from Ontario, New York State, and Quebec.
description: Lowe, D.G., Arnott, R.W.C., Chiarenzelli, J.R., and Rainbird, R.H. Early Paleozoic reactivation of a passive margin intra-plate rift: insights into reactivation of the Ottawa graben from detrital zircon provenance signatures of the Potsdam Group. Submitted to the Geological Society of America Bulletin.
DOI: 10.1594/ieda/100747
title: Paleoflow data from the Potsdam Group in Ontario, New York State, and Quebec

description: This dataset comprises paleoflow azimuth data from the Cambrian to Ordovician Potsdam Group in Ontario, New York State, and Quebec. It is intended to complement the GSA bulletin submission by Lowe et al. entitled "Early Paleozoic rifting and reactivation of a passive-margin rift: insights from detrital zircon provenance signatures of the Potsdam Group, Ottawa graben".
description: Lowe, D.G., Arnott, R.W.C., Chiarenzelli, J.R., and Rainbird, R.H. Early Paleozoic reactivation of a passive margin intra-plate rift: insights into reactivation of the Ottawa graben from detrital zircon provenance signatures of the Potsdam Group. Submitted to the Geological Society of America Bulletin.
DOI: 10.1594/ieda/100745
title: Geochemical, oxygen isotopic, and mineral age data of eclogite facies metapelites from the Sesia Zone (Western Alps, NW Italy)

description: Bulk geochemical analyses (XRF + LOI) of metapelites from the central Sesia Zone (Western Alps, NW Italy). Samples show eclogite facies assemblages and experienced re-hydration during Alpine subduction after previous de-hydration to granulite facies. The dataset shows that Sesia samples are derived from rocks related to Ivrea Zone granulites.
description: Engi, M., Giuntoli, F., Lanari, P., Burn, M., Kunz, B., & Bouvier, A.-S. (2018). Pervasive eclogitization due to brittle deformation and rehydration of subducted basement. Effects on continental recycling? Geochemistry, Geophysics, Geosystems
DOI: 10.1594/ieda/100743
title: Petrology Samples from the Submarine Tonga Arc Collected during the TELVE and NoToVE Cruises

description: This is a report describing petrological samples from the submarine Tonga Arc collected during the TELVE and NoToVE Cruises in 2003-2004 aboard the RV Southern Surveyor. This report derives from the original cruise report authored by Richard Arculus, and includes a detailed accounting of each dredge station (time and location on and off the bottom), and a description of each sample taken for petrological study. Geochemical data, including the primary dataset for volatile species in Tonga arc melt inclusions, are reported for a subset of these samples in Lauren Cooper's PhD Thesis (Boston University, 2009). This subset of samples are also registered in SESAR.
description: Lauren Cooper  (Ph.D.; Boston Univ., 2009) Volatiles in Tonga arc magmas and their role in unraveling subduction zone processes.

Cooper, L.B., Ruscitto, D., Plank, T., Wallace, P.J., Syracuse, E. and Manning, C.E. (2012)  Global Variations in H2O/Ce I: Slab Surface Temperatures beneath Volcanic Arcs. Geochem. Geophys. Geosyst. 13, Q03024, 27 PP., doi:10.1029/2011GC003902.

Cooper, L. B., T. Plank, R. J. Arculus, E. H. Hauri, P. S. Hall, and S. W. Parman (2010), High-Ca boninites from the active Tonga Arc, J. Geophys. Res., 115, B10206, doi:10.1029/2009JB006367.
DOI: 10.1594/ieda/100744
title: Calcium isotope data for bulk chondrules, chondrites and achondrites

description: This data set contains bulk rock, mass-dependent (42Ca/44Ca and 43Ca/44Ca) and mass-independent (48Ca/44Ca) calcium isotope compositions of chondrites (carbonaceous and ordinary) as well as terrestrial rock standards, lunar, Martian, ureilite, eucrite and angrite meteorites reported relative to the SRM 915b standard. Samples were analysed to investigate Solar System and planet formation processes. All data were produced by wet chemical analysis on a multi-collector inductively coupled plasma mass spectrometer following separation of calcium from its matrix through ion exchange chromatography.
description: M. Schiller, M. Bizzarro and V. A. Fernandes (2018),Isotopic evolution of the protoplanetary disk and the building blocks of Earth and Moon, Nature