Turbidite sequences within confined basins constitute important hydrocarbon reservoirs worldwide; for this reason the discrimination of sedimentary sub-environments based on an objective statistical method is of interest for pure and applied science. We investigated the potential use of the Hurst test (Chen & Hiscott 1999) as a statistical tool to discriminate sub-environments within geologically complex turbiditic units that fill a confined basin with well exposed facies transitions and onlaps, at the scale of several stacked reservoirs (Cengio and Bric la Croce - Castelnuovo Turbidite Systems in the Tertiary Piedmont Basin, Oligocene, Northern Italy). In vertical stratigraphic sections, the Hurst test determines the degree of clustering of low and high values of sedimentological variables like bed-thickness, grain-size and sand/mud ratio that are dependent on sub-environments of deposition. We applied the Hurst test to depocentral and marginal sub-areas across the basin (parallel and perpendicular to the main palaeo-current direction), documenting a different clustering of thick and thin beds, and of high and low values of the sand/mud ratio, in the depocentre-distal sector with respect to the onlap areas. A new field (onlap sub-environment) could thus be added to the Chen & Hiscott (1999) classification diagram of turbidite settings based on the Hurst index. The Hurst phenomenon i.e. clustering of high and low values of the selected variables, was also able to distinguish between proximal and distal (depocentral) lobe settings, and to recognize the fingerprint of the different depositional lobes (fully confined aggrading, prograding, backstepping). The map of turbidite sub-environments obtained by interpolation of the Hurst index is quite comparable to the field-observed facies map, providing impressive robust validation of the Hurst statistics. This method seems to represent a very promising predictive tool for subsurface studies of turbiditic oil fields based on core and log analyses.

Validation of Hurst statistics : a predictive tool to discriminate turbiditic sub-environments in a confined basin / F. Felletti, R. Bersezio. - In: PETROLEUM GEOSCIENCE. - ISSN 1354-0793. - 16:4(2010), pp. 401-412.

Validation of Hurst statistics : a predictive tool to discriminate turbiditic sub-environments in a confined basin

F. Felletti
Primo
;
R. Bersezio
Ultimo
2010

Abstract

Turbidite sequences within confined basins constitute important hydrocarbon reservoirs worldwide; for this reason the discrimination of sedimentary sub-environments based on an objective statistical method is of interest for pure and applied science. We investigated the potential use of the Hurst test (Chen & Hiscott 1999) as a statistical tool to discriminate sub-environments within geologically complex turbiditic units that fill a confined basin with well exposed facies transitions and onlaps, at the scale of several stacked reservoirs (Cengio and Bric la Croce - Castelnuovo Turbidite Systems in the Tertiary Piedmont Basin, Oligocene, Northern Italy). In vertical stratigraphic sections, the Hurst test determines the degree of clustering of low and high values of sedimentological variables like bed-thickness, grain-size and sand/mud ratio that are dependent on sub-environments of deposition. We applied the Hurst test to depocentral and marginal sub-areas across the basin (parallel and perpendicular to the main palaeo-current direction), documenting a different clustering of thick and thin beds, and of high and low values of the sand/mud ratio, in the depocentre-distal sector with respect to the onlap areas. A new field (onlap sub-environment) could thus be added to the Chen & Hiscott (1999) classification diagram of turbidite settings based on the Hurst index. The Hurst phenomenon i.e. clustering of high and low values of the selected variables, was also able to distinguish between proximal and distal (depocentral) lobe settings, and to recognize the fingerprint of the different depositional lobes (fully confined aggrading, prograding, backstepping). The map of turbidite sub-environments obtained by interpolation of the Hurst index is quite comparable to the field-observed facies map, providing impressive robust validation of the Hurst statistics. This method seems to represent a very promising predictive tool for subsurface studies of turbiditic oil fields based on core and log analyses.
turbidite systems ; confined basin ; Hurst test ; sandstone reservoirs ; Tertiary Piedmont Basin ; quantitative sedimentology.
Settore GEO/02 - Geologia Stratigrafica e Sedimentologica
2010
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/146943
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