You are in the accessibility menu

Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/102988
Full metadata record
DC FieldValueLanguage
dc.contributor.advisorSáenz, Carlos Alberto Tello [UNESP]-
dc.contributor.authorSoares, Cleber José-
dc.date.accessioned2014-06-11T19:32:20Z-
dc.date.accessioned2016-10-25T19:31:17Z-
dc.date.available2014-06-11T19:32:20Z-
dc.date.available2016-10-25T19:31:17Z-
dc.date.issued2012-03-31-
dc.identifier.citationSOARES, Cleber José. Geocronologia por traço de fissão em apatitas de rochas alcalinas: comparação dos diferentes métodos de datação e calibração da dosimetria de nêutrons. 2012. 116 f. Tese (doutorado) - Universidade Estadual Paulista, Instituto de Geociências e Ciências Exatas, 2012.-
dc.identifier.urihttp://hdl.handle.net/11449/102988-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/102988-
dc.description.abstractExternal Detector Method is a widely used technique in Fission Track Thermochronology, FTT, in which two different minerals are concomitantly employed: spontaneous tracks are observed in apatite and the induced ones in the external detector muscovite. They show intrinsic differences in detection and etching properties that should be taken into account. In this work, new geometry factor values, g, in apatite were obtained by ρED/ρIS ratio and GQR values through the measurement of projected lengths. Five mounts, two of which were large area prismatic sections (Mn-1 and Mn-2, Durango apatite) and three samples composed of random orientation pieces (D-2 and D-3, Durango apatite and TF-42, from crystalline rock) have been used to determine the g-values. A side effect of applying EDM is that the value of the initial confined induced fission track, L0, is not measured in routine analyses. The L0-value is an important parameter to quantify with good confidence the degree of annealing of the fossil fission tracks in the unknown age sample, being essential for accurate thermal history modeling. The impact of using arbitrary L0- values on the inference sample thermal history was investigated and discussed. The L0- value can be measured for each sample as an extension of the ρED/ρIS ratio method for measuring g, which consists in simultaneously irradiating pre-annealed apatite grains and the EDM mount of the same sample. The ratio between densities of induced tracks in the muscovite and in the extra apatite mount gives the value of g. L0 is the mean length of the confined fission tracks measured in the extra apatite mount. Eight apatite samples from crystalline basement, with grains at random orientation, were used to determine the gvalues. The resultant average found (0.560.02) is statistically in agreement with the values found for... (Complete abstract click electronic access below)en
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)-
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)-
dc.format.extent116 f. : il., tabs.-
dc.language.isoeng-
dc.publisherUniversidade Estadual Paulista (UNESP)-
dc.sourceAleph-
dc.subjectDatação do traço de fissãopt
dc.subjectGeologia estratigráficapt
dc.subjectTermocronologiapt
dc.subjectApatitapt
dc.subjectTempo geológicopt
dc.subjectRochas igneas alcalinaspt
dc.titleGeocronologia por traço de fissão em apatitas de rochas alcalinas: comparação dos diferentes métodos de datação e calibração da dosimetria de nêutronsen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso aberto-
dc.identifier.filesoares_cj_dr_rcla.pdf-
dc.identifier.aleph000706506-
dc.identifier.capes33004137035P2-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

There are no files associated with this item.
 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.