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- W2000581211 abstract "A newly identified early Oligocene marine transgression across the Pisco Basin of southern Peru resulted in the deposition of at least 150 m of fossiliferous sandstones and siltstones, informally designated the Otuma formation. Basal sandstones can usually be recognized in the field by the presence of the gastropod, Turritella woodsi Lisson 1925. New stratigraphic data demonstrate that Cenozoic marine sediments were deposited in the Pisco Basin between about 41-34 Ma, 31-28 Ma, 25-16 Ma, 15-11 Ma, 10-5 Ma, and 4-2 Ma. Most sequence boundaries in the Pisco Basin coincide with compressional tectonic events and/or eustatic low stands of sea level. Una nueva transgresión marina ha sido recientemente identificada en la Cuenca Pisco, Sur del Perú. Este es el resultado de la deposición de por lo menos 150m de areniscas y limolitas fosiliferas, informalmente aquı́ designado como Formación Otuma. Las areniscas basales pueden usualmente ser reconocidas en el campo por la presencia del gastropodo Turritella woodsi Lisson, 1925. Nuevos datos estratigráficos demuestran que los sedimentos marinos Cenozoicos fueron depositados en la Cuenca Pisco entre 41-34 Ma, 31-28 Ma, 25-15Ma, 14-11 Ma, 10-5 Ma, y 4-2 Ma. Muchas de los lı́mites de las secuencias en la Cuenca Pisco coincide con eventos tectónicos compresionales y/o niveles bajos del mar." @default.
- W2000581211 created "2016-06-24" @default.
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- W2000581211 date "1998-05-01" @default.
- W2000581211 modified "2023-10-13" @default.
- W2000581211 title "Oligocene deposition and Cenozoic sequence boundaries in the Pisco Basin (Peru)" @default.
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- W2000581211 doi "https://doi.org/10.1016/s0895-9811(98)00014-5" @default.
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