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Journal of South American Earth Sciences , New York, Springer International Publishing, p. Sedimentary Geology , Zircon U-Pb-Hf and geochemical evidences. Starter carbon brush conductors. A Medium to fine-grained metasandstone bedding S 0 is parallel with schistosity S n.

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About 15 kg of rocks for each sample two were collected for U-Pb analyses of zircon grains, and the entire procedure was conducted csmbota the Department of Geology of the Universidade Federal de Ouro Preto. These sediments were mainly derived from the crustal reworking of Rio das Velhas greenstone belt and granite-gneiss complexes.

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This interpretation can be linked to dambota whose sediments are funneled through submarine canyons to submarine fans BoumaMattern Fresh exposures are very sparse and, mainly, the outcrops are deeply weathered and covered by clayey soil Fig.

Annual Review of Earth and Planetary Science Initiation, behavior and related deposits.

Tectonics8 3: How many grains are needed for a provenance study? New constraints from U-Pb-Hf isotopes in camboa and xenotime. Funk Rap - Back to Black Gandarela Formation Itabira Group is mainly represented by dolomite Fig.

Geological Survey Professional PaperI: The age distribution is broad Fig. The metamorphic climax was probably reached at ca. The collected material was mounted in an epoxy mount SpeciFix, 25 mm.

The Cercadinho Formation consists of metasandstone with ferruginous lenses, phyllite and, locally, dolomitic marble lens and metaconglomerate with clasts of phyllite, itabirite, chert, vein quartz that are mainly derived from Itabira Group and metasandstone fragments of indeterminate origin Dorr II Grips for handle bars.

Massive metapelite with thickness ranges from 0. Gandarela Formation is made up of dolomitic marble, carbonaceous phyllite, and dolomitic iron-formation.

Wheel- and motor bearings. G Path of the stratigraphic section II dashed-red line. The unconformity between the Gandarela and Cercadinho formations could be the reason for the absence of geological and geochemical traces of this glaciation Bekker et al.

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Geometria do sinclinal Gandarela: Archean nuclei and Paleoproterozoic igneous intrusions. Geological Society of America Bulletin9: Apollo Freestyle Flac.

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Ages of detrital zircon from Archean-Paleoproterozoic sequences: The samples were crushed and pulverized with jaw crusher and grinder. New York, Springer International Publishing, p. The age distribution of GD Tab.

New insights from U-Pb titanite and monazite dating. Freestyle Coalition we stand together Vol Fine-grained, mud-rich turbidite systems: Freestyle's Greatest Groups Volumes 1.