The Effect of the Depth of the Non-Conducting Layer on the Induced Magnetic Field at the Peruvian Dip Equator

The internal part of the geomagnetic daily variations at the Peruvian dip equator shows the presence of an anomaly in the earth conductivity. This anomaly is further investigated in the present work using the external and internal parts of those variations, found in a previous work. The field induce...

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Detalles Bibliográficos
Autores principales:	Osella, A.M., Duhau, S.
Formato:	JOUR
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00221392_v35_n7_p245_Osella
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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