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The Morro Solar Group (Spanish: Grupo Morro Solar) is a stratigraphic group of Mesozoic-aged sedimentary formations exposed near Lima, Peru. The groups formations more specifically of Berriasian and Valanginian age (Early Cretaceous) and overlies the Jurassic and underlies the Cretaceous . The Morro Solar Group is intruded by sills of andesitic composition. Together with the Casma and , the Morro Solar Group contains clastic volcanosedimentary material derivative of the Mesozoic . The formations of the group hosts mostly local fossils which do not have counterparts for biochronological correlation in other regions.

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  • Morro Solar Group (en)
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  • The Morro Solar Group (Spanish: Grupo Morro Solar) is a stratigraphic group of Mesozoic-aged sedimentary formations exposed near Lima, Peru. The groups formations more specifically of Berriasian and Valanginian age (Early Cretaceous) and overlies the Jurassic and underlies the Cretaceous . The Morro Solar Group is intruded by sills of andesitic composition. Together with the Casma and , the Morro Solar Group contains clastic volcanosedimentary material derivative of the Mesozoic . The formations of the group hosts mostly local fossils which do not have counterparts for biochronological correlation in other regions. (en)
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  • Morro Solar Group (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Falla_normal_Morro_Solar_Peru.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Salto_del_Fraile_Lima_Peru.jpg
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  • The seaward tilting of the strata of Salto del Fraile Fm. was caused by the Andean orogeny (en)
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  • Hauterivian (en)
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  • The Morro Solar Group (Spanish: Grupo Morro Solar) is a stratigraphic group of Mesozoic-aged sedimentary formations exposed near Lima, Peru. The groups formations more specifically of Berriasian and Valanginian age (Early Cretaceous) and overlies the Jurassic and underlies the Cretaceous . The Morro Solar Group is intruded by sills of andesitic composition. Together with the Casma and , the Morro Solar Group contains clastic volcanosedimentary material derivative of the Mesozoic . The formations of the group hosts mostly local fossils which do not have counterparts for biochronological correlation in other regions. (en)
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