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The major sedimentological features of R&#237;o Turbio deposits that pertain lo the Austral Argentinian Basin are <i>herein dealt with the sequence as established there consists</i> of a marine environment (Cerro Dorotea Formation), giving way to a vastly fluctuating shoreline coastal deposits (Rio Turbio Formation), unconformably overlain by continental sediments (Cerro Mirador conglomerates and Rio Guillermo Formation).  Environment wise local variation (foreshore, backshore, tidal channel, tidal plain, braided drainage...) fits a three megacycle pattern each one evolving through a complex succession of lesser cycles, which are but a reflection of minor transgressive-regressive phases.  En este trabajo, se analizan las principales caracter&#237;sticas sedimentol&#243;gicas de los dep&#243;sitos del &#225;rea de r&#237;o Turbio, en la Cuenca Austral Argentina.  Se determina la <i>existencia de dep&#243;sitos marinos</i> (F. Cerro Dorotea) a los que se superponen dep&#243;sitos t&#237;picos de zona litoral, con frecuentes oscilaciones de la l&#237;nea de costa (F. R&#237;o Turbio), terminando con dep&#243;sitos continentales discordantes sobre ellos. (F. R&#237;o Guillermo y Conglomerados Cerro Mirador).  Los dep&#243;sitos caracterizados son muy variados (foresbore, backsbore, canales tidales, llanuras mareales, &#225;reas fluviales, etc.), orden&#225;ndose en tres megaciclos, cuya estructura interna presenta una complicada sucesi&#243;n de ciclos de menor rango, que suelen corresponder a peque&#241;as etapas transgresivas y regresivas

Caracterización sedimentológica del área de Río Turbio, Cuenca Austral (provincia de Santa Cruz. Republica Argentina)