Apreciação Geológica e Petrográfica de algumas rochas básicas de Santos

dc.creatorPichler, Ernesto
dc.creatorCampos, João Ernesto de Souza
dc.date1955-12-17
dc.date.accessioned2022-12-15T20:58:07Z
dc.date.available2022-12-15T20:58:07Z
dc.identifierhttps://ppegeo.igc.usp.br/index.php/bffcluspmineralogia/article/view/10745
dc.identifier10.11606/bmffclusp.v0i13.121463
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5362933
dc.descriptionIn the present paper the authors present some data on the geology of Santos considering particularly the occurrences of basic rocks. The geologic map shows the main occurrences of these rocks, indicating their respective geologic coordinates. A rather detailed petrographic study of rocks, sampled at the occurences of São Vicente and ilha Porchat, revealed that the first one was a lam prophyric dike with a high percentage of olivine whereas the rock of the ilha Porchat was classified as diabase. It is the opinion of the authors that these occurrences originated at different geologic times, and that the olivinic rocks of São Vicente, whose origin is likely to be connected with the epeirogenic movem ents of the serra do mar, are younger than the diabase of the ilha Porchaten-US
dc.formatapplication/pdf
dc.languagepor
dc.publisherUniversidade de São Paulo. Faculdade de Filosofia, Letras e Ciências Humanaspt-BR
dc.relationhttps://ppegeo.igc.usp.br/index.php/bffcluspmineralogia/article/view/10745/10221
dc.rightsDireitos autorais 2016 Boletim. Mineralogia - Faculdade de Filosofia, Ciências e Letras, Universidade de São Paulopt-BR
dc.sourceBoletim da Faculdade de Filosofia, Ciências e Letras da Universidade de São Paulo. Mineralogia; n. 13 (1955); 57-68pt-BR
dc.source0372-4824
dc.titleApreciação Geológica e Petrográfica de algumas rochas básicas de Santosen-US
dc.titleApreciação Geológica e Petrográfica de algumas rochas básicas de Santospt-BR
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArtigo Avaliado pelos Parespt-BR


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