SciELO - Scientific Electronic Library Online

 
vol.6 número3FILTRO DE POLARIZACIÓNSVD TENIENDO EN CUENTA LA PLANARIDAD DE LA ENERGÍA DE GROUND ROLLCOMPARACIÓN DE INDICADORES DE FUENTE DE CRUDOS BASADOS EN PARÁMETROS DE C15-, C15+ YC40+. índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • En proceso de indezaciónCitado por Google
  • No hay articulos similaresSimilares en SciELO
  • En proceso de indezaciónSimilares en Google

Compartir


CT&F - Ciencia, Tecnología y Futuro

versión impresa ISSN 0122-5383

Resumen

LOPEZ-RAMOS, Eduardo. HYDROCARBON GENERATION MODELS ALONG THE BASAL DETACHMENT OF THE ANDEAN SUBDUCTION ZONE IN NORTHERN ECUADOR TO SOUTHERN COLOMBIA. C.T.F Cienc. Tecnol. Futuro [online]. 2016, vol.6, n.3, pp.25-52. ISSN 0122-5383.

ABSTRACT Numerous fluid vents and hydrocarbon seeps of a thermogenic origin have been reported in the middle and lower slope of the Northern Ecuadorean - Southern Colombian (NESC) Pacific margin. These hydrocarbon manifestations are frequently located over the traces of faults connected with the basal detachment of the subduction zone, very far (80km) from the hydrocarbon kitchens formed along the axis of the NESC forearc basins. In some subduction zones, the origin of these types of thermogenic seeps is related to the generation and migration of hydrocarbons along the subduction zone décollement. To test the possibility of generation of hydrocarbons in the NESC décollement, 2D Time-Temperature Index Arrhenius equation (TTIArr) numerical models were constructed in four regional cross sections. The results suggest that along the top of the subducting plate, favorable conditions exist for oil and gas generation below depths of 10 km , with subtle variations of the oil and gas depths of generation, due to lateral changes in the thermal structure of the margin. The available geophysical data support the presence of favorable structures to trap the hydrocarbons generated along the top of the subducting plate (low velocity zones), and/or the seepage of fluids to the sea floor along the middle and lower slope of the NESC margin.

Palabras clave : Subduction plane; Hydrocarbons; 2DTTIArr; Low velocity zones.

        · resumen en Español | Portugués     · texto en Inglés     · Inglés ( pdf )