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dc.contributor.author
Rapalini, Augusto Ernesto  
dc.contributor.other
Siegesmund, Siegfried  
dc.contributor.other
Basei, Miguel A. S.  
dc.contributor.other
Oyhantzabal, Pedro  
dc.contributor.other
Oriolo, Sebastián  
dc.date.available
2025-04-24T10:59:00Z  
dc.date.issued
2018  
dc.identifier.citation
Rapalini, Augusto Ernesto; The Assembly of Western Gondwana: Reconstruction Based on Paleomagnetic Data; Springer; 2018; 3-18  
dc.identifier.isbn
978-3-319-68919-7  
dc.identifier.uri
http://hdl.handle.net/11336/259452  
dc.description.abstract
In the last two decades some consensus has been reached with regard to the assembly of Gondwana being a long and complex process. Reliable paleomagnetic data are essential to determine the paleogeographic and kinematic evolution of each Gondwana-forming block during its assembly as well as to place chronological constraints on such a process. A review of paleomagnetic data from Western Gondwana blocks indicates that the available Ediacaran to Cambrian database is still scarce and uneven for different cratons, despite clear improvement in the quantity and quality of paleomagnetic information in recent decades. The main constraints placed by the available information are as follows:The Río de la Plata and Congo Sao Francisco cratons were likely already attached by mid-Ediacaran times (c. 575 Ma) and not part of Rodinia.The Arabian-Nubian Shield was part of proto-Gondwana by 550 Ma and probably even earlier.Paleomagnetic constraints are virtually absent for the Kalahari craton.Amazonia and West Africa were probably still part of Rodinia and attached to eastern Laurentia by the Early Ediacaran (c. 615 Ma), suggesting that a large Ediacaran Clymene Ocean existed between Amazonia and the Congo Sao Francisco Río de la Plata block.The age of Amazonia amalgamation is poorly constrained by paleomagnetic data as ≥525 Ma.The accretion of Eastern Gondwana blocks probably occurred in the latest Ediacaran-Cambrian times as suggested by the apparent polar wander path of Australia.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Springer  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Gondwana  
dc.subject
Paleomagnetism  
dc.subject
apparent polar wander path  
dc.subject
Precambrian  
dc.subject.classification
Geociencias multidisciplinaria  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS  
dc.title
The Assembly of Western Gondwana: Reconstruction Based on Paleomagnetic Data  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.type
info:eu-repo/semantics/bookPart  
dc.type
info:ar-repo/semantics/parte de libro  
dc.date.updated
2025-04-24T10:22:17Z  
dc.journal.pagination
3-18  
dc.journal.pais
Suiza  
dc.description.fil
Fil: Rapalini, Augusto Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-68920-3_1  
dc.conicet.paginas
688  
dc.source.titulo
Teh Geology of southwestern Gondwana