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Tofalo, O.; Morras, H.; Sanchez-Bettucci, L., E-mail: rtofalo@gl.fcen.uba.ar
The III working days of the Cenozoic2012
The III working days of the Cenozoic2012
AbstractAbstract
[en] The Fray Bentos formation is composed by loessic deposits based on paleosoils and pedogenic calcretes (Oligocene - early miocene). In this deposits are tubular and lamellar formations which would have been formed in arid climates.The fluvial origen of Raigon Formation, (late pliocene and middle pleistocene) presents a paleosoil roof which is generated under a subhumid climate.The Libertad Formation during the glacial intervals consisted of loess deposits
Original Title
Paleosuelos y calcretes pedogenicos de las formaciones Fray Bentos (Oligoceno-Mioceno temprano), Raigon (Plioceno tardio-Pleistoceno medio) y Libertad (Pleistoceno temprano a medio)
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Sociedad Uruguaya de Geologia, Montevideo (Uruguay); [5.65 Mb]; Jun 2012; p. 1-5; Geology working day; Jornadas de geologia; Montevideo (Uruguay); 14-15 Jun 2012; Lecture
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