Camilo AristizabalLAMCE-LAB2M COPPE-UFRJ · Engineering
Camilo Aristizabal
Geologist MSc., PhD.
About
27
Publications
4,711
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48
Citations
Citations since 2017
Introduction
Marine Geologist and Geophysicist. Geophysical information interpreter as seismic and potential data
Additional affiliations
July 2015 - present
Position
- Senior Researcher
Description
- Seismic Modeling and Interpretation of whole spectrum of geophysical and geological data, Geochemical Analysis and Petrophysics
July 2015 - present
PETREC
Position
- Senior Geologist
July 2015 - present
LAB2M-LAMCE
Position
- Explorationl Geologist
Education
January 2009 - January 2013
March 2006 - October 2008
August 1994 - April 2003
Publications
Publications (27)
Resumen Con el análisis de imágenes Landsat y trabajo de campo en varios lugares del norte de la Sierra Nevada de Santa Marta y la península de La Guajira, se han encontrado evidencias de tectónica activa. Igualmente la Red Sismológica Nacional de Colombia (RSNC), registra sismicidad para esta región, la cual es periódica con 3.0 ≤ M L ≤ 5.0 al igu...
Resumen Con el análisis de imágenes Landsat y trabajo de campo en varios lugares del norte de la Sierra Nevada de Santa Marta y la península de La Guajira, se han encontrado evidencias de tectónica activa. Igualmente la Red Sismológica Nacional de Colombia (RSNC), registra sismicidad para esta región, la cual es periódica con 3.0 ≤ M L ≤ 5.0 al igu...
Coupled fission-track and U–Pb analyses of detrital zircons are presented. A Cretaceous intracratonic basin formed between 93 to 60 Ma, the Bauru Basin, is investigated to distinguish its provenance and information about the main orogenetic events of the South American Platform. The results of U–Pb zircon dating suggest that Rhyacian (Transamazonia...
In Espírito Santo State, Brazil, between Vitória, Colatina and Ecoporanga, there is a shear zone which trends NNW-SSE and is filled by a diabase dyke swarm named the Vitória-Ecoporanga Dyke Swarm (VEDS).
South of the VEDS, offshore, the Vitória Structural High (VSH) represents an elevated basement region which
bounds the Campos and Espírito Santo b...
Caracterizar as estruturas do embasamento sob os depósitos sedimentares do CDRPS, visando diferenciar eventos tectônicos rifte e pós-rifte.
Intracratonic basins usually record the polyhistory of cratons or plates during the deposition
time as well as the remote geological time. Fission-track (FT) combined with U-Pb in situ analyses of
detrital zircons thus reveals the polyhistory of this type of basin. To distinguish the crustal accretion of
the South American Platform, 29 sandstone sa...
A diffuse low deep microseismicity located overall between the Guajira peninsula and the Sierra Nevada de Santa Marta (SNSM) was registered with the recent installation (2008 to Present) of three seismological stations in northeastern Colombia by the Colombian Seismological Network (RSNC), but mainly with the Uribia station in (the) central region...
Seismological records and geologic observations along the entire coastal zone of Cartagena and surroundings, northern Colombia, have been interpreted as a result of the deformation and sedimentary processes caused by E-W right directional transpressive regional tectonics. In this case study, it was identified a close relationship between diapiric f...
Start from analysis of LANDSAT images with field check in several places toward north of the Sierra Nevada de Santa Marta and the La Guajira peninsula we found active tectonics evidences. In same manner the Colombian seismological network called as Red Sismológica Nacional de Colombia (RSNC), and the Global Seismological Network (NEIC) had been reg...
Desde la instalación en la década de 1990 de la Red Sismológica Nacional de Colombia (RSNC) se ha observado una sismicidad periódica con 3.0 ≤ ML ≤ 5.0 que se ubica hacia la región central y sur de la península de la Guajira y hacía la parte central y suroriental de la Sierra Nevada de Santa Marta. Igualmente la red sismológica mundial (NEIC) ha lo...
De acordo com o registo da Rede sismológica Nacional da Colômbia (RSNC), tem se observado sismicidade periódica com 3.0 ≤ ML ≤ 5.0, a qual se localiza na região central e sul da Península de La Guajira e na porção central e sudeste da Serra Nevada de Santa Marta. Infelizmente esta rede sismológica possui um número muito pequeno de estações na regiã...
The results obtained by inversion of fracture and striae structural data shows that there is a main compressive stress field with an horizontal 1 striking approximately N15-30E. It is compatible with a transcurrent binary of right-lateral strike slip indicating dextral movement to the VCE Dike Swarm along the N20W structural corridor. Intrusion of...
In order to get a better understanding of the hydrogeological behavior of the region by
using Vertical Electrical Sounding (VES), and aiming an optimization of resources housed in the aquifers, a geological and geophysical characterization were made on the bedrock aquifer located in the Barro Branco Sub-Basin, northern of Rio de Janeiro State (Braz...
The north Colombian continental edge tectonic framework is related to the Nazca/South American/Caribbean Plates triple junction. The seismological records and the geology of the Cartagena city and neighborhoods have been interpreted as a result of the deformation and sedimentary processes caused by NW direction regional compressive tectonics. The s...
Con base en el estudio geomorfológico de la zona costera del Departamento de La Guajira – Colombia, se describieron indicios de levantamiento activo relacionados con la Falla de Oca, en la margen continental del Norte suramericano. La falla limita por el Norte el bloque estructural triangular que conforma la Sierra Nevada de Santa Marta (SNSM). Los...
Projects
Projects (6)
Altos estruturais e/ou vulcânicos, de natureza e extensão geográficas distintas, separam as bacias de Santos, Campos e Espírito Santo e afetam diretamente as 3 áreas. De sul para norte, a bacia de Pelotas é separada da bacia de Santos por um complexo vulcano-estrutural – o Alto de Florianópolis-Dorsal de São Paulo; enquanto o Alto de Cabo Frio é outro lineamento vulcano-estrutural que define o limite norte da bacia de Santos e sul da bacia de Campos. Já o limite sul da bacia do Espírito Santo (limite norte da bacia de Campos) é, para finalidades legais, definido pelo Alto de Vitória. Estes altos estruturais tiveram papel importante na segmentação estrutural e sedimentar destas bacias, provavelmente desde o início da fase rifte.
Deste modo, o principal objetivo desta proposta é a investigação da evolução tectono-sedimentar destes principais altos estruturais da margem continental sudeste brasileira, focalizando na sua influência sobre o registro e a arquitetura sedimentar das bacias marginais de Santos, Campos e Espírito Santo.
Project about application of methodologies and inversion techniques that uses innovative technologies by analysis of elastic properties of rocks for digital petrophysics analysis and quantitative seismic interpretation.
