Geological, pedological and paleomagnetic study of the late Cenozoic sedimentary sequence in southwestern Uruguay, South America

The results of interdisciplinary studies carried out on the coastal cliffs of southern Uruguay are presented here. The Raigón Formation (late Pliocene-middle Pleistocene) has a cratonic provenance and comprises two sections limited by a regional discontinuity. Each section is composed of an associat...

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Detalles Bibliográficos
Autores principales:	Tofalo, O.R., Orgeira, M.J., Morrás, H., Vásquez, C., Sánchez, L., Pecoits, E., Aubet, N., Sánchez, G., Zech, W., Moretti, L.
Formato:	JOUR
Materias:	Cenozoic cliff climate variation craton discontinuity floodplain geochronology interdisciplinary approach lithofacies magnetostratigraphy paleoclimate paleogeography paleomagnetism paleosol pedogenesis pedology Pliocene-Pleistocene boundary provenance rhizolith sedimentary sequence sedimentation stratification South America Uruguay
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_10406182_v210_n1-2_p6_Tofalo
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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