Please use this identifier to cite or link to this item: http://hdl.handle.net/1822/33770

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dc.contributor.authorRodrigues, Benedito C.por
dc.contributor.authorPeternell, Markpor
dc.contributor.authorMoura, Antóniopor
dc.contributor.authorSchwindinger, Martinpor
dc.contributor.authorPamplona, J.por
dc.date.accessioned2015-02-10T14:57:03Z-
dc.date.available2015-02-10T14:57:03Z-
dc.date.issued2012-
dc.identifier.urihttp://hdl.handle.net/1822/33770-
dc.description.abstractThe internal structure of a shearband boudin resulting from an original igneous, hydrothermal or metamorphic segregation tabular rigid body is a subject of scientific interest. It allows understanding the deformation mechanisms acting on homogeneous quartz aggregate activated during simple shear progressive deformation. This work is focused on the characterization of the internal evolution of shearband boudins, using microtextural analysis, fluid inclusions studies, fractal and OCP analysis. The proposed interpretative model shows the several structural stages that can be well established during the process of the internal evolution of shearband boudin.por
dc.language.isoengpor
dc.rightsopenAccesspor
dc.subjectShearband boudinpor
dc.subjectHT ductile shear zonepor
dc.subjectMicrotextural analysispor
dc.subjectFluid inclusions studiespor
dc.subjectFractal and OCP analysispor
dc.titleInterpretative model of shearband boudins internal evolution in HT ductile shear zonespor
dc.typeconferenceAbstract-
dc.peerreviewedyespor
sdum.publicationstatuspublishedpor
oaire.citationConferenceDate26 Mar. – 01 Abr. 2012por
sdum.event.typeconferencepor
oaire.citationStartPage85por
oaire.citationEndPage85por
oaire.citationConferencePlaceKiel, Alemanhapor
oaire.citationTitleSymposium Tectonics, Structural Geology and Geology of crystalline rocks (TSK14)por
dc.subject.fosCiências Naturais::Ciências da Terra e do Ambientepor
sdum.conferencePublicationSymposium Tectonics, Structural Geology and Geology of crystalline rocks (TSK14)por
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