columna estratigráfica del cusco

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  • 8/20/2019 columna estratigráfica del cusco

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         F     A     N     E

         R     O     Z     O     I     C     O

    MIOCENO

    INFERIOR

    EOCENO

         M     E     S      O      Z     O      I     C      O 

    JURASICO   MEDIO

    TRIASICO

    SUPERIOR

         C      E     N     O      Z     O      I     C      O 

    PALEOGENO

    MEDIO

    CRETACICO

    NEOGENO

    INFERIOR

         P     A     L     E     O     Z     O     I     C     O

    MEDIO

    FORMACION ANANEA

    SUPERIOR

    PALEOCENO

    INFERIOR

    MISSISIPIANO

    DEVONICO

    FORMACION ENE

    SUPERIOR

    PLEISTOCENO

    CARBONIFERO

    INFERIOR

    PLIOCENO

    SUPERIOR

    PERMICO

    PENSILVANIANO

    FORMACION CAICAY

    SILURICO

    OLIGOCENO

                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                          G                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       R                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       U                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       P                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       O                

                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                           M                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       I                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                       T

                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                           U                

    CUATERNARIO

    F. HUANCANE

    PRIDOLI

    FORMACION PISAC

    F. PARURO

    LOPINGIANO

    F. PUQUIN

    FORMACION CHILCA

    FORMACION CCATCA

    LUDLOW

    CISULARIANO

    F. PACHATUSAN

    GUADALUPANO

    HOLOCENO

    WENLOCK

    FORMACION PACCARITAMBO

    FORMACION RUMICOLCA

    FORM. HUAMBUTIO

    F. KAYRA

    F. SONCCO

    M2

    F. SAN SEBASTIAN

    FORMACION CHINCHEROS

    M2

    M 1

    FORMACION QUILQUE

    LLANDOVERY

    M3

    M1

    SUPERIOR

    INF.

    M1

    M2

    GRUPO COPACABANA

    INFERIOR

    MED.

    FORMACION PUNACANCHA

    F. PAUCARBAMBA

    FORMACION AYABACAS

    FORMACION MARAS

    SUP.

    GRUPO

    SAN

    JERONIMO

    GRU-

    PO

    YUN-

    CAY-

    PATA

    COLUMNA ESTRATIGRAFICA DE LA REGION DEL CUSCO