1997
DOI: 10.1029/97jb01143
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Quantifying lateral heterogeneities in fluvio‐deltaic sediments using three‐dimensional reflection seismic data: Offshore Gulf of Mexico

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Cited by 14 publications
(18 citation statements)
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“…They concluded that the fluvial sediments (with high‐amplitude channels trending north‐northwest) in one horizontal plane were consistent with FBM with H ≈ 0.4 to 0.65 in roughly the direction of channels (along dip) and H ≈ 0.05 transverse to the channels (along strike). Deshpande et al [1997] found less striking evidence of horizontal anisotropy in the deltaic sediments, with different H values of 0.26 versus 0.4. All of their vertical data was in the FBM range, with H ≈ 0.3 to 0.5.…”
Section: Operator‐scaling Random Fieldsmentioning
confidence: 77%
“…They concluded that the fluvial sediments (with high‐amplitude channels trending north‐northwest) in one horizontal plane were consistent with FBM with H ≈ 0.4 to 0.65 in roughly the direction of channels (along dip) and H ≈ 0.05 transverse to the channels (along strike). Deshpande et al [1997] found less striking evidence of horizontal anisotropy in the deltaic sediments, with different H values of 0.26 versus 0.4. All of their vertical data was in the FBM range, with H ≈ 0.3 to 0.5.…”
Section: Operator‐scaling Random Fieldsmentioning
confidence: 77%
“…Following [11][12][13][14][15][16][17][18][19][20][21], statistical scaling of moments of velocity is investigated through the analysis of directional sample structure functions, i.e., qth-order statistical moments of absolute increments…”
Section: Scaling Of Statisticsmentioning
confidence: 99%
“…Indeed, the statistics of hydrological properties in aquifers and reservoirs exhibit dependences on various characteristic length scales, e.g., measurement volume and resolution, scale of observation, spatial correlation, and size of the sampled domain [10]. Scaling analyses of statistical moments of hydraulic conductivity and permeability data have been presented in many works, including [11][12][13][14][15][16][17][18][19][20]. In all these studies, measurement volumes are associated with a support scale ranging from the millimeter to the meter and data sets are collected on domains at the field (kilometer) or laboratory (decimeter to meter) scale.…”
Section: Introductionmentioning
confidence: 99%
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“…Porosity logs from 15 wells drilled in a deltaic environment in the Gulf of Mexico give a spectral slope of 1.4 with a standard deviation of 0.2 [ Pelletier and Turcotte , 1996]. However, within the same basin, vertical geophysical well logs of a multifacies sand/shale deposit from a fluvial/deltaic system give a spectral slope ranging from 1.4 to 2.1 [ Deshpande et al , 1997], higher than the other data and falling outside the range of 1/ f noise.…”
Section: Discussionmentioning
confidence: 99%