Suíte vulcânica serra da bocaina, grupo amoguijá, maciço rio apa-MS

• Autor(a) principal: Godoy, Antonio Misson [UNESP]
• Data de Publicação: 2010
• Outros Autores: Manzano, Jefferson Cassu [UNESP], de Araújo, Larissa Marques Barbosa, da Silva, Jesué Antonio
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Repositório Institucional da UNESP
• Texto Completo: http://geociencias.no-ip.org/29_4/Art%2011_Godoy.pdf; http://hdl.handle.net/11449/72125
• topic: Lithogeochemistry; Petrography; Rio apa massif; Serra da bocaina volcanic suite; andesite; craton; igneous intrusion; ignimbrite; outcrop; petrography; Proterozoic; pumice; quartz; rhyolite; sediment chemistry; tuff; Brazil; Mato Grosso do Sul

The Rio Apa Massif corresponds to the southeastern portion of the Amazonian Craton and crops out in the Mato Grosso do Sul State, Brazil. It is constituted by rocks of paleoproterozoic age of Rio Apa Complex, Alto Tererê Group and the plutonic-volcanic suites of the Amoguijá Group, subdivided in Alumiador Intrusive suits and Serra da Bocaina Volcanic. The Volcanic Suite is represented by São Francisco and Bocaina mountains and is constituted by terms of the composition of alkali - rhyolitic to rhyolitic, including in minor amounts riodacite, andesite and dacite. It consists of a variety of textual subvolcanic rocks, volcanic and varied volcanoclastics. The pyroclastic deposits are very expressive and consist of pyroclastic particle immerse in aphanitic matrix, fine grained or amorphous, where quartz, feldspar, chlorite, sericite, microlithes of carbonate, sparse spherulites and reliquiar volcanic glass can be distinguished. The pyroclastic rocks are represented by breccias, ignimbrites, agglomerate, tuffs, lapillistones and pumices and contain commonly vitroclasts, lithoclasts and crystalloclasts, pumices, fiammes, glass shards, spherulites, vesicles and amygdales. They are calc-alkaline rocks with dominant peraluminous character high to middle potassium series and define a sin-colisional dominant tectonic and are genetically associated to the evolution of the Amoguijá Magmatic Arc.