Early cretaceous absolute geomagnetic paleointensities from Cordoba Province (Argentina)
We present here new paleointensity and geochronology results from Early Cretaceous volcanic rocks of Sierra Chica de Cordoba (Argentina). The new K-Ar isotopic ages of 5 samples range from 136 to 122 Ma. Twenty five samples from 7 individual flows yielded acceptable paleointensity estimates. The mea...
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2006 |
| País: | México |
| Institución: | Universidad Nacional Autónoma de México |
| Repositorio: | Sistema de Información de la Facultad de Ciencias, UNAM |
| OAI Identifier: | oai:repositorio.fciencias.unam.mx:11154/2315 |
| Acceso en línea: | http://hdl.handle.net/11154/2315 |
| Access Level: | acceso abierto |
| Palabra clave: | Geosciences, Multidisciplinary paleointensity rock-magnetism Early Cretaceous South America |
| Sumario: | We present here new paleointensity and geochronology results from Early Cretaceous volcanic rocks of Sierra Chica de Cordoba (Argentina). The new K-Ar isotopic ages of 5 samples range from 136 to 122 Ma. Twenty five samples from 7 individual flows yielded acceptable paleointensity estimates. The mean paleointensity values per flow are ranging from 53.0 +/- 1.9 to 25.4 +/- 2.6 mu T and the corresponding Virtual Dipole Moments (VDMs) are ranging, from 9.3 +/- 1.3 to 4.6 +/- 0.5 (10(22) Am-2). This corresponds to the mean value of 7.3 +/- 1.7 x 10(22) Am-2, which is compatible to the present geomagnetic axial dipole. Currently available selected paleointensity data from 80 to 130 Ma suggest that geomagnetic field strength frequently fluctuated before and during the Cretaceous Normal Superchron while the magnetic polarity maintained stable. The mean paleointensities derived from Cordoba lavas agree remarkably well with those obtained from the Parana Magmatic Province (133-132 Ma). This reinforces the hypothesis about the unreliability of 'Mesozoic Dipole Low'. |
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