The use of the magnetic signal of soils and paleosoils as a climatic function

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The use of the magnetic signal of soils and paleosoils as a climatic function. The correlation between an index of potential water storage (PWS) with magnetic signal in soils and paleosoils, developed in loessic sediments has been proposed. The analyzed data suggest the existence of climatic thresho...

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Detalles Bibliográficos
Autores principales:	Orgeira, M.J., Compagnucci, R.H.
Formato:	JOUR
Materias:	Late cenozoic Magnetism Paleoclimate Paleosoils Cenozoic geomagnetism loess magnetic mineral paleoclimate paleosol parent material Rumania
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v65_n4_p612_Orgeira
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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