On the origin and tectonic significance of the intra-plate events of Grenvillian-type age in South America: A discussion

• Autor(a) principal: CORDANI, Umberto G.
• Data de Publicação: 2010
• Outros Autores: FRAGA, Leda Maria Barreto, REIS, Nelson, TASSINARI, Colombo C. G., NEVES, Benjamin Bley Brito
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: Repositório Institucional de Geociências - RIGEO
• Texto Completo: https://rigeo.cprm.gov.br/handle/doc/572
• topic: TECTÔNICA; CINTURÕES OROGÊNICOS; CRÁTON AMAZÔNICO; CRÁTON SÃO FRANCISCO; AMÉRICA DO SUL

The objective of this article is to examine the available evidence of intra-plate tectonic episodes of "Grenvillian-type age", affecting the South-American continent, assessing their possible causal correlation with the tectonic processes occurring within the orogenic belts active at their margins. For the Amazonian Craton, the active margin is represented by the Rondonian-San Ignacio and Sunsas belts. However, active margins of similar age are not recognized for the São Francisco and the Rio de La Plata Cratons, and the intra-plate events over them could be reflections of the Kibaran, Irumide or Namaqua orogenic collisions in Africa. Grenvillian-type age events over the Amazonian Craton can be described in four different aspects: shearing and tectonic reactivation along zones of weakness, cratogenic granitic magmatism, alkaline ring complexes, and pervasive regional heating in some localized regions. The first of them may reflect the compressional stresses at active margins, however the others may have different origins