Revised mesozoic apw path for south america (1993)
- Autor:
- Autor USP: ERNESTO, MARCIA - IAG
- Unidade: IAG
- Subjects: GEOFÍSICA; PALEOMAGNETISMO
- Language: Inglês
- Imprenta:
- Publisher place: Buenos Aires
- Date published: 1993
- Source:
- Título: Abstracts. Division i
- Conference titles: International Association of Geomagnetism and Aeronomy Scientific Assembly
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ABNT
ERNESTO, Márcia. Revised mesozoic apw path for south america. 1993, Anais.. Buenos Aires: Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, 1993. . Acesso em: 14 fev. 2026. -
APA
Ernesto, M. (1993). Revised mesozoic apw path for south america. In Abstracts. Division i. Buenos Aires: Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo. -
NLM
Ernesto M. Revised mesozoic apw path for south america. Abstracts. Division i. 1993 ;[citado 2026 fev. 14 ] -
Vancouver
Ernesto M. Revised mesozoic apw path for south america. Abstracts. Division i. 1993 ;[citado 2026 fev. 14 ] - Temporal and spatial characteristics of the Paraná Magmatic Province: inferences from paleomagnetism and magnetic fabric
- A non-plume origin for the Paraná Magmatic Province (Southern Brazil): constraints from geochemical, isotopic, geochronological and geophysical data
- Caracteristicas texturais, estruturais e de anisotropia magnetica dos minerios de ferro da mina do andrade (joao monlevade, mg)
- 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?
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