SciELO - Scientific Electronic Library Online

 
vol.64 número3Sucesión volcánica Jurásica en el área de Charcas, San Luis Potosí: Contribución al entendimiento del Arco Nazas en el noreste de MéxicoAnormalidades morfológicas y enanismo en foraminíferos del Maastrichtiano de la Formación Cárdenas, plataforma Valles-San Luis Potosí: evidencias de estrés paleoambiental índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Boletín de la Sociedad Geológica Mexicana

versión impresa ISSN 1405-3322

Resumen

QUILANTAN PEDRAZA, Antonio  y  REYES SANCHEZ, Marcos Antonio. Petrophysic characterization of Neogene sand in a gas-producing well of the Veracruz Basin. Bol. Soc. Geol. Mex [online]. 2012, vol.64, n.3, pp.295-304. ISSN 1405-3322.

To know the output potential of hydrocarbons in a reservoir and its optimization, it is necessary to apply different engineering disciplines. One important discipline is petrophysics, which carries out the petrophysical characterization of the reservoir at a static level, and determines the physical properties of the rocks and types of fluids present in the reservoir, mainly porosity, permeability, grain size, and pore and fluid saturation. To determine the petrophysical properties, a geophysical log evaluation is carried out, integrating core data. Five horizons with gas potential were identified at the study area at the Neogene level, which include seven types ofpetrophysical rock types and thirteen flow units. The petrophysical description helped to re-evaluate the reserves and define the rock types and flow units that contribute to production, as well as to identify the areas with output potential in sandy horizons correlated with the study area.

Palabras llave : Log evaluation; petrophysical rock type and flow units.

        · resumen en Español     · texto en Español     · Español ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons