Chilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidation

Chilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidation

dc.creatorCorrêa-Gomes, LC.
dc.creatorSouza, M.N.
dc.creatorCorreia, D.R.
dc.date1991-12-01
dc.date.accessioned2022-12-15T19:41:10Z
dc.date.available2022-12-15T19:41:10Z
dc.identifierhttps://ppegeo.igc.usp.br/index.php/bigsp/article/view/1346
dc.identifier10.11606/issn.2317-8078.v0i10p09-15
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5358273
dc.formatapplication/pdf
dc.languageeng
dc.publisherUniversidade de São Paulo, Instituto de Geociênciaspt-BR
dc.relationhttps://ppegeo.igc.usp.br/index.php/bigsp/article/view/1346/1235
dc.rightsDireitos autorais 2016 Boletim IG-USP. Publicação Especialpt-BR
dc.sourceBoletim IG-USP. Publicação Especial; n. 10 (1991): II Workshop on Mafic Dyke Swarms of Brazil; 09-15pt-BR
dc.source2317-8078
dc.source0102-6275
dc.titleChilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidationen-US
dc.titleChilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidationpt-BR
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typept-BR


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