On the reliability of Mesozoic Dipole Low: New absolute paleointensity results from Paraná Flood Basalts (Brazil)

Geophysical Research Letters

Volumn 29, Issue 13, 2002, Pages 33-1-33-4

  Goguitchaichvili, Avto ^a   Alva Valdivia, Luis M ^a   Urrutia, Jaime ^a   Morales, Juan ^a   Lopes, Omar Ferreira ^b  

^a UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO   (Mexico)

^b FEDERAL UNIVERSITY OF PARANÁ   (Brazil)

Author keywords

[No Author keywords available]

Indexed keywords

BASALT; GEOMAGNETISM; RELIABILITY;

DIPOLE MOMENTS;

GEOPHYSICS;

FLOOD BASALT; GEOMAGNETISM; MAGNETIC INTENSITY; MESOZOIC; PALEOMAGNETISM;

BRAZIL; PARANA STATE;

EID: 0036662812     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2002GL015242     Document Type: Article

References (14)

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4. The intensity of the Earth's magnetic field over the past 160 million years
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6. Paleointensity of the Earth magnetic field for the past 400 My: Evidence for a dipole structure during the Mesozoic low
7. Intensity of the Earth's magnetic field: Evidence for a Mesozoic dipole low
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13. Sur l'intensité du champ magnétique terrestre dans le passé historique et géologique
14. Geomagnetic paleointensity just prior to the Cretaceous normal superchron