dc.creator | Correa-Gomes, LC | |
dc.creator | Oliveira, EP | |
dc.date | 2000 | |
dc.date | JUL | |
dc.date | 2014-12-02T16:30:00Z | |
dc.date | 2015-11-26T16:43:36Z | |
dc.date | 2014-12-02T16:30:00Z | |
dc.date | 2015-11-26T16:43:36Z | |
dc.date.accessioned | 2018-03-28T23:28:41Z | |
dc.date.available | 2018-03-28T23:28:41Z | |
dc.identifier | Gondwana Research. Elsevier Science Bv, v. 3, n. 3, n. 325, n. 332, 2000. | |
dc.identifier | 1342-937X | |
dc.identifier | WOS:000088002900003 | |
dc.identifier | 10.1016/S1342-937X(05)70291-4 | |
dc.identifier | http://www.repositorio.unicamp.br/jspui/handle/REPOSIP/58785 | |
dc.identifier | http://www.repositorio.unicamp.br/handle/REPOSIP/58785 | |
dc.identifier | http://repositorio.unicamp.br/jspui/handle/REPOSIP/58785 | |
dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1273647 | |
dc.description | Several mafic dyke swarms of similar composition and age (tholeiite- ca.1.0 Ga) occur on both sides of the Atlantic Ocean in eastern South America and western Africa. When assembled to their pre-drift position in the Mesozoic, the Brazilian coastal dyke province of Bahia, and the African dykes in Cameroun (Ebolowa suite) and Congo (Comba and Sembe-Ouesso provinces) define a giant radiating pattern (1200 km x 800 km) similar to other dyke swarms elsewhere associated with large-scale continental rifting. Magma flow indicators of the Brazilian dykes and branching propagation styles of their African counterparts indicate that the dyke conduits were fed with magmas diverging from a source beneath the long axis of the Meso-Neoproterozoic West-Congolian Basin in Africa. There, MORE-like metabasalts have been described in the La Bikossi Group of the Mayombian Supergroup. Whether the rifting event and intrusion of dyke swarms were triggered or not by a mantle plume beneath part of the Rodinia subcontinental lithosphere remain to be confirmed. | |
dc.description | 3 | |
dc.description | 3 | |
dc.description | 325 | |
dc.description | 332 | |
dc.language | en | |
dc.publisher | Elsevier Science Bv | |
dc.publisher | Amsterdam | |
dc.publisher | Holanda | |
dc.relation | Gondwana Research | |
dc.relation | Gondwana Res. | |
dc.rights | fechado | |
dc.rights | http://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy | |
dc.source | Web of Science | |
dc.subject | mafic dykes | |
dc.subject | palaeocontinental reconstruction | |
dc.subject | Rodinia supercontinent | |
dc.subject | Pan-african | |
dc.subject | Congo | |
dc.subject | Dolerites | |
dc.subject | Margins | |
dc.title | Radiating 1.0 Ga mafic dyke swarms of eastern Brazil and western Africa: Evidence of post-assembly extension in the rodinia supercontinent? | |
dc.type | Artículos de revistas | |