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Titlebook: Geology and Tectonics of Northwestern South America; The Pacific-Caribbea Fabio Cediel,Robert Peter Shaw Book 2019 Springer Nature Switzerl

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https://doi.org/10.1007/978-3-642-20456-2, including metaigneous and metasedimentary blocks of the disjointed and reworked paleo-autochthon, fragments of pericratonic and possibly exotic oceanic margin, and late, autochthonous siliciclastic and volcanic sequences, each reflecting distinct development stages in the complex plate dynamics of the Northern Andean paleo-margin.
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The Romeral Shear Zone, including metaigneous and metasedimentary blocks of the disjointed and reworked paleo-autochthon, fragments of pericratonic and possibly exotic oceanic margin, and late, autochthonous siliciclastic and volcanic sequences, each reflecting distinct development stages in the complex plate dynamics of the Northern Andean paleo-margin.
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1863-4621 s relationship with the Pacific Plate, Caribbean Plateau and.This book provides a comprehensive overview of the geological evolution of the Northern Andes and contiguous shield areas, with a focus upon Colombia. Updated geological interpretations are supported by modern lithogeochemical, seismic, gr
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https://doi.org/10.1007/978-3-642-21052-5ean orogeny. Tectonic consolidation and subduction of the segmented Nazca Plate during the late Miocene-Pliocene led to conformation of the modern-day Colombian segment of the Northern Andean Volcanic Zone. The Colombian arc segment represents the northernmost expression of subduction-related volcanism within South America’s Andean Cordillera.
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Late Cenozoic to Modern-Day Volcanism in the Northern Andes: A Geochronological, Petrographical, andean orogeny. Tectonic consolidation and subduction of the segmented Nazca Plate during the late Miocene-Pliocene led to conformation of the modern-day Colombian segment of the Northern Andean Volcanic Zone. The Colombian arc segment represents the northernmost expression of subduction-related volcanism within South America’s Andean Cordillera.
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Book 2019. Updated geological interpretations are supported by modern lithogeochemical, seismic, gravity and magnetic data and radiogenic isotope and radiometric age determinations. The composite data permits a detailed interpretation of the tectono-magmatic history of the Northern Andean Block, including th
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Morphotectonic and Orogenic Development of the Northern Andes of Colombia: A Low-Temperature Thermocory of the Northern Andes of Colombia using detailed compilations and analysis of existing LTTC datasets, in an effort to define the spatial distribution, timing, and magnitude of the main orogenic phases in the region, while providing an up-to-date morphotectonic picture of the Northern Andes.
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Proterozoic Basement, Paleozoic Tectonics of NW South America, and Implications for Paleocontinentalver was “transferred” to southern Mexico in Late Paleozoic time. Permian magmatic belts running along active margins in Mexico and northern South America place a time limit for this connection at the onset of the assemblage of Pangea.
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The Proterozoic Basement of the Western Guiana Shield and the Northern Andesth to the Guajira Peninsula in the north, and continues further northeast into Venezuela and eastwards into the Subandean basins. The Andean basement consists mainly of granulites and other high-grade metamorphic rocks, mainly of supracrustal origin, as well as minor plutons, formed during the Grenv
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