New data on the dynamics of the Scope of the Santander Massif during the Secondary (Eastern Cordillera of Colombia)
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Universidad Industrial de Santander
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Se analiza la tendencia positiva del área del Macizo de Santander durante la etapa de sedimentación mesozoica en el ámbito de la Cordillera Oriental. Esta tendencia positiva queda registrada por el adelgazamiento de las series y existencia de lagunas estratigráficas en el Macizo y por la distribución de facies en el cretácico inferior condicionada en varios aspectos por la existencia de la zona umbral del Macizo de Santander.
It is analyzed the positive tendency of the area of the Santander Massif during the Mesozoic sedimentation in the Cordillera Oriental. This positive tendency remain registered by a thinner Cretaceous and the existenceship of breakes in the Cretaceous sequence on the Santander Massif, and by the distribution of facies in the Lower Cretaceous.
It is analyzed the positive tendency of the area of the Santander Massif during the Mesozoic sedimentation in the Cordillera Oriental. This positive tendency remain registered by a thinner Cretaceous and the existenceship of breakes in the Cretaceous sequence on the Santander Massif, and by the distribution of facies in the Lower Cretaceous.