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dc.contributor.CRUESPUNIVERSIDADE ESTADUAL DE CAMPINASpt_BR
dc.contributor.authorunicampVerma, Sanjeet Kumar-
dc.typeArtigopt_BR
dc.titleA new computer program tecdia for multidimensional tectonic discrimination of intermediate and acid magmas and its application to the Bohemian Massif, Czech Republicpt_BR
dc.contributor.authorVerma, Surendra P.-
dc.contributor.authorCruz-Huicochea, Rene-
dc.contributor.authorDiaz-Gonzalez, Lorena-
dc.contributor.authorVerma, Sanjeet K.-
dc.subjectRochas ígneaspt_BR
dc.subjectGeoquímicapt_BR
dc.subjectPetrogênesept_BR
dc.subjectGeologia estruturalpt_BR
dc.subject.otherlanguageIgneous rockspt_BR
dc.subject.otherlanguageGeochemistrypt_BR
dc.subject.otherlanguagePetrogenesispt_BR
dc.subject.otherlanguageGeology, Structuralpt_BR
dc.description.abstractA new computer program TecDIA written in Java, for the application of 35 previously-defined multidimensional diagrams for the tectonomagmatic discrimination of intermediate and acid magmas is briefly described. A detailed Readme document is presented in the Supplementary Electronic Material file. As an innovation, this program provides a ready to publish report containing a synthesis of all diagrams, including the total percent probabilities. The use of this program is illustrated by two examples of the Bohemian Massif ( Czech Republic) for older Carboniferous (granitoids of the Central Bohemian Pluton) and younger Late Carboniferous-Early Permian igneous rocks (volcanics from late Variscan continental basins and granitoids of the Zulova Pluton). According to the results, the tectonic setting for the Early Carboniferous rocks was collisional, whereas for the Late Carboniferous-Early Permian igneous suite it was either a collision or a transition from collisional to a within-plate setting. The acid rocks probably dominated by a crustal component may provide a somewhat different result as compared to the intermediate rocks. TecDIA freely available from http://tlaloc.ier.unam.mx will certainly be useful for all interested in applying these 35 multidimensional diagramspt_BR
dc.relation.ispartofJournal of Geosciencespt_BR
dc.publisher.cityPraguept_BR
dc.publisher.countryRepública Checapt_BR
dc.publisherCeska Geologicka Spolecnostpt_BR
dc.date.issued2015-
dc.language.isoengpt_BR
dc.description.volume60pt_BR
dc.description.issuenumber4pt_BR
dc.description.firstpage203pt_BR
dc.description.lastpage218pt_BR
dc.rightsFechadopt_BR
dc.sourceWOSpt_BR
dc.identifier.issn1802-6222pt_BR
dc.identifier.eissn1803-1943pt_BR
dc.identifier.doi10.3190/jgeosci.201pt_BR
dc.identifier.urlhttp://www.jgeosci.org/detail/jgeosci.201pt_BR
dc.description.sponsorshipFUNDAÇÃO DE AMPARO À PESQUISA DO ESTADO DE SÃO PAULO - FAPESPpt_BR
dc.description.sponsordocumentnumber2012/07243-3; 12/15824-6pt_BR
dc.date.available2020-12-22T12:12:51Z-
dc.date.accessioned2020-12-22T12:12:51Z-
dc.description.provenanceSubmitted by Cintia Oliveira de Moura (cintiaom@unicamp.br) on 2020-12-22T12:12:51Z No. of bitstreams: 0. Added 1 bitstream(s) on 2021-02-19T18:59:56Z : No. of bitstreams: 1 000368189800001.pdf: 776490 bytes, checksum: 4fbac0f74d3c4ec2c9728cda8d5fe265 (MD5)en
dc.description.provenanceMade available in DSpace on 2020-12-22T12:12:51Z (GMT). No. of bitstreams: 0 Previous issue date: 2015en
dc.identifier.urihttp://repositorio.unicamp.br/jspui/handle/REPOSIP/353372-
dc.contributor.departmentsem informaçãopt_BR
dc.contributor.unidadeInstituto de Geociênciaspt_BR
dc.identifier.source000368189800001pt_BR
dc.creator.orcid0000-0002-4390-5147pt_BR
dc.type.formArtigopt_BR
dc.description.sponsorNotePrograma de Apoyo a Proyectos de Investigacion e Innovacion Tecnologica (PAPIIT)pt_BR
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