Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay

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The continental deposits found in southern and western Uruguay show important climatic changes along the Cenozoic. The sequence begins with Paleocene palustrine carbonates known as the Queguay Formation, associated with calcretes of phreatic origin which developed mainly on fluvial sediments of Merc...

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Detalles Bibliográficos
Autores principales:	Tófalo, O.R., Morrás, H.J.M.
Formato:	JOUR
Materias:	Duricrusts Paleoclimates Paleosols Siliciclastic sedimentites climate variation duricrust fluvial deposit loess Miocene Paleocene paleoclimate paleosol pedogenesis Pleistocene siliciclastic deposit Uruguay
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v65_n4_p674_Tofalo
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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