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dc.contributor.authorParcerisa Duocastella, David
dc.contributor.authorRossell Garriga, Josep Maria
dc.contributor.authorFàbrega Alsina, Carles
dc.contributor.authorGurenko, Andrey
dc.contributor.authorFranke, Christine
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Minera, Industrial i TIC
dc.date.accessioned2017-03-14T08:49:57Z
dc.date.available2017-03-14T08:49:57Z
dc.date.issued2017-02
dc.identifier.citationParcerisa Duocastella, D. [et al.]. (2017). Predicting instrumental mass fractionation (IMF) of stable isotope SIMS analyses by response surface methodology (RSM) [Dataset]. 1 v. Universitat Politècnica de Catalunya. https://doi.org/10.5821/data-2117-102417-1
dc.identifier.urihttp://hdl.handle.net/2117/102417
dc.descriptionThe dataset contains four files. File S1 corresponds to cathodoluminescence and BSE images of standard minerals. File S2 contains geochemical data of mineral standards ans samples obtained by SIMS and EPMA. File S3 contains the parameters used to obtain response surface models of IMF in mineral standards. File S4 is a response surface methodology tutorial.
dc.description.abstractInstrumental mass fractionation (IMF) of isotopic SIMS analyses (Cameca 1280HR, CRPG Nancy) was predicted by response surface methodology (RSM) for 18O/16O determinations of plagioclase, K-feldspar and quartz. The three predictive response surface models combined instrumental and compositional inputs. The instrumental parameters were: (i) X and Y position, (ii) LT1DefX and LT1DefY electrostatic deflectors, (iii) chamber pressure and, (iv) primary-ion beam intensity. The compositional inputs included: (i) anorthite content (An%) for the plagioclase model and, (ii) orthoclase (Or%) and barium (BaO%) contents for the K-feldspar model. The three models reached high predictive powers. The coefficients R2 and prediction-R2 were, respectively, 90.47% and 86.74% for plagioclase, 87.56% and 83.17% for K-feldspar and 94.29% and 91.59% for quartz. The results show that RSM can be confidently applied to IMF prediction in stable isotope SIMS analyses by the use of instrumental and compositional variables.
dc.language.isoeng
dc.publisherUniversitat Politècnica de Catalunya
dc.relation.ispartofhttp://hdl.handle.net/2117/100911
dc.relation.ispartofhttp://hdl.handle.net/2117/103444
dc.relation.ispartofhttp://hdl.handle.net/2117/114114
dc.relation.ispartofhttp://hdl.handle.net/2117/170191
dc.rightsCC0 1.0 Universal
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Mineralogia
dc.subject.otherGeochemistry
dc.titlePredicting instrumental mass fractionation (IMF) of stable isotope SIMS analyses by response surface methodology (RSM) [Dataset]
dc.typeDataset
dc.contributor.groupUniversitat Politècnica de Catalunya. CoDAlab - Control, Modelització, Identificació i Aplicacions
dc.contributor.groupUniversitat Politècnica de Catalunya. GREMS - Grup de Recerca en Mineria Sostenible
dc.identifier.doi10.5821/data-2117-102417-1
dc.rights.accessOpen Access
dc.description.version1
dc.relation.projectidinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PGC2018-093903-B-C22/ES/CIRCULACION DE FLUIDOS DURANTE LA EVOLUCION DE CUENCAS INVERTIDAS Y CINTURONES OROGENICOS: APLICACION EN EL ALMACENAMIENTO DE CO2/
local.ispartof.titleFàbrega, C., Parcerisa, D., Rossell, Josep M., Gurenko, A., Franke, C. Predicting instrumental mass fractionation (IMF) of stable isotope SIMS analyses by response surface methodology (RSM). "Journal of analytical atomic spectrometry", 10 Febrer 2017.
local.ispartof.titleParcerisa Duocastella, D. [et al.]. (2016). Geostandards of the Valentí Masachs Geology Museum [Dataset]. 1 v. Universitat Politècnica de Catalunya. https://doi.org/10.5821/data-2117-103444-1
local.ispartof.titleFàbrega, C. [et al.]. (2018). Geochemical data of albitized profiles in Europe [Dataset]. 1 v. Universitat Politècnica de Catalunya.
local.ispartof.titleFàbrega, C. [et al.]. Permian–Triassic red-stained albitized profiles in the granitic basement of NE Spain: evidence for deep alteration related to the Triassic palaeosurface. "International journal of Earth sciences", 1 Octubre 2019, vol. 108, núm. 7, p. 2325-2347.


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