Titlebook: Cretaceous Tectonics of the Andes; José A. Salfity Book 1994 Springer Fachmedien Wiesbaden 1994 Evolution.Geodynamic.Kreide.Sediment

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https://doi.org/10.1007/978-3-658-07974-1 Colombian East and the Colombian West occurred during the end of the Cretaceous or beginning of the Cenozoic, with large-scale lateral displacement along the Otú-Pericos fault. This movement continued later along the Cauca-Romeral system that crosses the tectono-metamorphic structures formerly crea

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https://doi.org/10.1007/978-3-658-07974-1an” phase starts with a paleogeographic change probably triggered by the incipient coastal uplift (Turonian-Coniacian boundary), and continues in the Late Coniacian-Early Santonian with the initiation of northeastward overthrusts located at the southwestern boimdary of the western Trough. It culmina

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uplifts upon which younger fine-grained strata onlapped. The oldest and most important extensional episode took place during deposition of the lowermost part of the Puca Group (Condo conglomerates). A younger minor extensional episode developed locally, possibly in Late Neocomian and/or Aptian time

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The Colombian Andes During Cretaceous Times, Colombian East and the Colombian West occurred during the end of the Cretaceous or beginning of the Cenozoic, with large-scale lateral displacement along the Otú-Pericos fault. This movement continued later along the Cauca-Romeral system that crosses the tectono-metamorphic structures formerly crea

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Kimmeridgian to Paleocene Tectonic and Geodynamic Evolution of the Peruvian (and Ecuadorian) Marginan” phase starts with a paleogeographic change probably triggered by the incipient coastal uplift (Turonian-Coniacian boundary), and continues in the Late Coniacian-Early Santonian with the initiation of northeastward overthrusts located at the southwestern boimdary of the western Trough. It culmina

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Kimmeridgian? to Paleocene Tectonic Evolution of Bolivia, uplifts upon which younger fine-grained strata onlapped. The oldest and most important extensional episode took place during deposition of the lowermost part of the Puca Group (Condo conglomerates). A younger minor extensional episode developed locally, possibly in Late Neocomian and/or Aptian time

TOXIC

Tectono-Sedimentary Evolution of the Cretaceous-Early Tertiary and Metallogenic Scheme of Northern ian) and “Incaic” (during the Eocene-Oligocene transition) tectonic phases..In connection with these succesive periods of magmatic and tectonic activity a series of important metallogenic processes developed, both linked to volcanic and post-plutonic hydrothermal phases, which gave rise to the follo