Drift of South American platform since early cretaceous: reviewing the apparent polar wander path (2006)
- Autor:
- Autor USP: ERNESTO, MARCIA - IAG
- Unidade: IAG
- Subjects: PALEOMAGNETISMO; CRETÁCEO
- Language: Inglês
- Imprenta:
- Source:
- Título: Geociências
- ISSN: 0101-9082
- Volume/Número/Paginação/Ano: v. 25, n. 1, p. 83-90, 2006
-
ABNT
ERNESTO, Márcia. Drift of South American platform since early cretaceous: reviewing the apparent polar wander path. Geociências, v. 25, n. 1, p. 83-90, 2006Tradução . . Acesso em: 14 mar. 2026. -
APA
Ernesto, M. (2006). Drift of South American platform since early cretaceous: reviewing the apparent polar wander path. Geociências, 25( 1), 83-90. -
NLM
Ernesto M. Drift of South American platform since early cretaceous: reviewing the apparent polar wander path. Geociências. 2006 ; 25( 1): 83-90.[citado 2026 mar. 14 ] -
Vancouver
Ernesto M. Drift of South American platform since early cretaceous: reviewing the apparent polar wander path. Geociências. 2006 ; 25( 1): 83-90.[citado 2026 mar. 14 ] - Temporal and spatial characteristics of the Paraná Magmatic Province: inferences from paleomagnetism and magnetic fabric
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- Defining a South American reference mean paleomagnetic pole for the permo-carboniferous reversed superchron
- Paleomagnetismo do enxame de diques ceara-mirim, nordeste do brasil
- New paleomagnetic data on the cretaceous intrusive rocks related to the serra geral formation, southern brazil
- Holocene secular variation from lake sediments reassessed
- 'ANTPOT.40 AR' / 'ANTPOT.39 AR' dating of the ponta grossa dike swarm (brazil), and implications to parana flood volcanism
- Paleomagnetic constraints on the age of the Botucatu formation in Rio Grande do Sul, Southern Brazil
- Millenial-scale quasi-periodicities recorded at permocarboniferous rhythmites (Paraná Basin, Brazil): are 'bond cycles' a permanent features throughout the Phanerozoic?
- Spectral analysis of paleozoic magnetostratigraphic time series: recognition of millenial scale climatic forcing parameters
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