Petrology and geochemistry of a megacrystic quartz monzonite, the Bodocó pluton, northeastern Brazil

dc.creatorMcMurry, Jude
dc.date.accessioned2016-11-14T23:13:10Z
dc.date.available2011-02-18T19:26:44Z
dc.date.available2016-11-14T23:13:10Z
dc.date.issued1991-05
dc.description.abstractThe coarse-grained Bodoco pluton is characterized by tabular megacrysts of K-feldspar in a matrix of plagioclase, hornblende, biotite, titanite, and quartz. The pluton is reversely zoned from a partly granitic and granodioritic margin to a voluminous quartz monzonitic (QMZ) core. Within the pluton, elongated km-wide zones of deformed, foliated megacrystic QMZ are associated with synplutonic dikes of dark gray monzonite and monzodiorite. Limited exposures of a topographically high region of the pluton have a hybridized texture in which felsic and mafic compositions are complexly intermingled.
dc.format.mimetypeapplication/pdf
dc.identifier.urihttp://hdl.handle.net/2346/10802en_US
dc.language.isoeng
dc.publisherTexas Tech Universityen_US
dc.rights.availabilityUnrestricted.
dc.subjectMonzoniteen_US
dc.subjectIntrusionsen_US
dc.titlePetrology and geochemistry of a megacrystic quartz monzonite, the Bodocó pluton, northeastern Brazil
dc.typeDissertation

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