Sebastián Echeverri

ORCID: 0000-0003-1147-0756
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About
Contact & Profiles
Research Areas
  • Geological and Tectonic Studies in Latin America
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • Geological and Geophysical Studies Worldwide
  • International Relations in Latin America
  • Comparative constitutional jurisprudence studies
  • Geological Studies and Exploration
  • Aviation Industry Analysis and Trends
  • Political Dynamics in Latin America
  • Business, Innovation, and Economy
  • Archaeological Research and Protection
  • Maritime and Coastal Archaeology
  • Transportation Planning and Optimization
  • Air Traffic Management and Optimization
  • Cultural and political discourse analysis
  • Reservoir Engineering and Simulation Methods
  • Archaeology and ancient environmental studies
  • Migration, Racism, and Human Rights

Universidad Nacional de Colombia
2018-2025

University of Caldas
2012-2023

Universidade de São Paulo
2015-2019

Abstract Andean orogenic processes controlled the spatial and temporal distribution of magmatic sedimentary record. This contribution integrates new U/Pb zircon ages, heavy mineral analyses biostratigraphic constraints from Neogene record fore‐arc intra‐arc basins volcano‐plutonic rocks southwestern Colombia, to reconstruct these processes. The results reveal continuous arc magmatism since Late Oligocene, with a major post‐Middle Miocene peak exhumation. When integrated other geological...

10.1111/ter.12167 article EN Terra Nova 2015-06-13

Marginal basins are the result of extensional tectonics along convergent margins. These include an early stage seafloor spreading that, in some cases, is followed by tectonic inversion and deformation basin formation a new magmatic arc front. The Early Cretaceous South American Plate caused development multiple pre-Andean back-arc marginal continental margin. were inverted during onset Andean orogeny Late Cretaceous. For instance, Northern Andes, remnants this history found Central...

10.1080/00206814.2025.2462928 article EN International Geology Review 2025-02-13

The Combia Volcanic Province (~11-5 Ma), is a volcaniclastic sequence located in northwest Colombia between the Central and Western cordilleras at 5-6° N latitude. Its source associated with volcanic activity of magmatic arc produced by subduction Nazca plate under South American northern Andes. distribution, composition, chronostratigraphy province’s deposits are well-known, sequences characterized as compositionally bimodal. older rocks (ca. 11-9 Ma) display tholeiitic affinity, whereas...

10.5027/andgeov50n2-3503 article EN cc-by Andean geology 2023-06-07

RESUMENEl conocimiento estratigráfico del relleno sedimentario segmento onshore de la cuenca ante-arco Tumaco es poco conocido y los trabajos existentes se fundamentan en el estudio líneas sísmicas pozos para exploración hidrocarburos, haciendo énfasis las unidades más superficiales.Se presenta detallado rocas Mioceno superior -Plioceno expuestas sector sur Tumaco.Los nuevos datos estratigráficos pozo ANH-Tumaco 1-ST-S representan sección completa mejor preservada este intervalo tiempo.Se...

10.18273/revbol.v38n4-2016003 article ES cc-by Boletín de Geología 2016-06-01

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10.2139/ssrn.4778236 preprint EN 2024-01-01

Volcanic stratigraphy provides major insights to understand the spatial and temporal relationships between volcanic products eruptive post-eruptive processes. In Andean chain, Neogene modern magmatic arc front has shown changes in their compositional characteristics, which have been commonly related significant modifications plate configuration. northern segment of Colombian Andes, at 5°N latitude, a series Upper Miocene-Pliocene volcaniclastic units record tectono-magmatic evolution...

10.1080/00206814.2024.2444583 article EN cc-by-nc-nd International Geology Review 2024-12-31

La integracion de la informacion estratigrafica del relleno sedimentario cenozoico cuenca antearco Tumaco, basada en los pozos exploratorios perforados el segmento onshore, permite identificar tres megasecuencias con rangos edades desde Eoceno hasta Plioceno. megasecuencia Eoceno-Oligoceno, dominantemente lutitica, es considerada como intervalo generador hidrocarburos esta cuenca. Mioceno temprano-Mioceno medio y tardio-Plioceno, constituidas por sucesiones arenosas menor proporcion...

10.3997/2214-4609-pdb.330.171 article ES 11th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas 2012-07-29

Grajales et al. (2020) reviewed geochronological and geochemical data from Paleogene volcanic plutonic rocks outcropping in the Panama-Choco Block (north western Cordillera) southern Western Cordillera, as well Central Cordillera of Colombia. These were used to support a model continuous arc magmatism along Colombian continental margin, propose paleogeographic for arc. The authors did not discuss previously published paleomagnetic, geochemical, geochronological, thermochronological...

10.22201/cgeo.20072902e.2021.2.1615 article EN Revista Mexicana de Ciencias Geológicas 2021-07-21
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