dc.contributorUniversidade Estadual Paulista (UNESP)
dc.creatorIyer, S. S.
dc.creatorde Oliveira, M. A F
dc.creatorHoefs, J.
dc.creatorKrouse, H. R.
dc.date2014-05-27T11:17:28Z
dc.date2016-10-25T18:12:56Z
dc.date2014-05-27T11:17:28Z
dc.date2016-10-25T18:12:56Z
dc.date1992-07-01
dc.date.accessioned2017-04-06T00:43:59Z
dc.date.available2017-04-06T00:43:59Z
dc.identifierJournal of South American Earth Sciences, v. 6, n. 1-2, p. 59-66, 1992.
dc.identifier0895-9811
dc.identifierhttp://hdl.handle.net/11449/64243
dc.identifierhttp://acervodigital.unesp.br/handle/11449/64243
dc.identifier10.1016/0895-9811(92)90017-S
dc.identifier2-s2.0-0027072574
dc.identifierhttp://dx.doi.org/10.1016/0895-9811(92)90017-S
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/886144
dc.descriptionSulfur and carbon isotope compositions of ten scapolites from granulite-facies rocks of the São José do Rio Pardo area, Guaxupé Complex, Brazil, were measured. Scapolite is the primary and major rock-forming mineral in these rocks (up to 40 volume %). The isotopic composition of the sulfate and carbonate group in the scapolite structure has δ34S values of +1.0‰ to +6.7‰, and δ13C values of -14.3‰ to -6.3‰, respectively. The sulfur isotope data may be related to an upper mantle (external) or lower crustal (internal) source for the sulfur, whereas the carbon appears to have been derived from an internal source. Thus, the carbon and sulfur isotope data can be explained without invoking an external (mantle) source. © 1993.
dc.languageeng
dc.relationJournal of South American Earth Sciences
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectcarbon
dc.subjectgranulite
dc.subjectisotopic composition
dc.subjectscapolite
dc.subjectsulphur
dc.subjectBrazil, Sao Jose do Rio Pardo
dc.titleSulfur and carbon isotopes in scapolite-bearing granulites of the São José do Rio Pardo area, Brazil
dc.typeOtro


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