TY - JOUR
T1 - Lacunarity of geophysical well logs in the Cantarell oil field, Gulf of Mexico
AU - Arizabalo, Rubén Darío
AU - Oleschko, Klavdia
AU - Korvin, Gabor
AU - Lozada, Manuel
AU - Castrejón, Ricardo
AU - Ronquillo, Gerardo
PY - 2006
Y1 - 2006
N2 - Lacunarity and fractal variations in geophysical well logs are associated with stratigraphic and petrophysical properties of the naturally fractured Cantarell field in the Gulf of Mexico. Neutron porosity (NPHI), density (RHOB, DRHO, PEF), resistivity (LLD, LLS, MSFL), natural radioactivity (GR, CGR, URAN, POTA, THOR) and caliper (CALI) logs are studied. The resistivity logs yielded remarkably high lacunarity values, especially in the hydrocarbon source- and reservoir rocks. Lacunarity ∧ was found to depend on the resolution and radial depth of penetration of the logging method. It systematically increased in the following order: ∧(RHOB) < ∧(CALI) < ∧(PEF) < ∧(URAN) < ∧(GR) < ∧(NPHI) < ∧(POTA) < ∧(CGR) < ∧(THOR) < ∧(MSFL) < ∧(DRHO) < ∧(LLS) < ∧(LLD).
AB - Lacunarity and fractal variations in geophysical well logs are associated with stratigraphic and petrophysical properties of the naturally fractured Cantarell field in the Gulf of Mexico. Neutron porosity (NPHI), density (RHOB, DRHO, PEF), resistivity (LLD, LLS, MSFL), natural radioactivity (GR, CGR, URAN, POTA, THOR) and caliper (CALI) logs are studied. The resistivity logs yielded remarkably high lacunarity values, especially in the hydrocarbon source- and reservoir rocks. Lacunarity ∧ was found to depend on the resolution and radial depth of penetration of the logging method. It systematically increased in the following order: ∧(RHOB) < ∧(CALI) < ∧(PEF) < ∧(URAN) < ∧(GR) < ∧(NPHI) < ∧(POTA) < ∧(CGR) < ∧(THOR) < ∧(MSFL) < ∧(DRHO) < ∧(LLS) < ∧(LLD).
KW - Fractal analysis
KW - Lacunarity
KW - R/S method
KW - Scaling
KW - Self-similarity
KW - Well logs
UR - https://www.scopus.com/pages/publications/33750013521
U2 - 10.22201/igeof.00167169p.2006.45.2.185
DO - 10.22201/igeof.00167169p.2006.45.2.185
M3 - Article
AN - SCOPUS:33750013521
SN - 0016-7169
VL - 45
SP - 99
EP - 113
JO - Geofisica International
JF - Geofisica International
IS - 2
ER -