--> Seismic Geomorphology by Spectral Decomposition Volume Interpretation for Basin-Scale Depositional System Delineation, Cuyo Group, Argentina
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AAPG ACE 2018

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Previous HitSeismicNext Hit Geomorphology by Spectral Decomposition Volume Previous HitInterpretationNext Hit for Basin-Scale Depositional System Delineation, Cuyo Group, Argentina

Abstract

Spectral decomposition analyzes a given signal by the summation of simple, well defined basis functions. The spectral content of Previous HitseismicNext Hit Previous HitdataNext Hit is influenced by the acoustic properties in the Earth, and therefore significant information can be gained from the analysis of the Previous HitseismicNext Hit at different frequencies through spectral decomposition during Previous HitseismicNext Hit Previous HitinterpretationNext Hit (Partyka G. et al, 1999). The ability to examine and compare the response at different frequency bands is critical to obtain information that otherwise is difficult to visualize on the full bandwidth Previous HitdataNext Hit (Chopra et al, 2007). Volumetric RGB (Red-Green-Blue) blend of the optimum frequency cubes (Hall and Trouillot, 2004) rapidly assess and highlight the presence of geological features present in the Previous HitseismicNext Hit Previous HitdataNext Hit. Previous HitSeismicNext Hit geomorphology facilitates the study of the subsurface by the extraction of geomorphologic insights from 3D Previous HitseismicNext Hit Previous HitdataNext Hit (Posamentier et al, 2005).

The Cuyo group is an Early to Middle Jurassic siliciclastic sedimentary sequence in the Neuquén basin western Argentina, bounded by two regional unconformities (Intra Liassic & Intra Callovian at base & top respectively) that reaches 2500 meters of thickness and includes several transgressive-regressive cycles associated to thermal subsidence, the paleo-Pacific ocean connection and a continuous contribution of sediments (Dellapé et al, 1979).

3D Previous HitseismicNext Hit and chronostratigraphic regional Previous HitinterpretationNext Hit (nine sedimentary cycles) for the Cuyo Group were conditioned for spectral decomposition, as Previous HitseismicNext Hit Previous HitdataNext Hit quality and Previous HitinterpretationNext Hit have significant impact in the results. Individual surveys (+20) were analyzed and regionally integrated.

Canyons filled with channels of different geometries and sizes are clearly identified in the slope, while fans are observed in the deep water area. Previous HitSeismicNext Hit geomorphology using spectral decomposition volume based Previous HitinterpretationNext Hit allows the connection of channels in the platform, canyons in the slope and fans in the deep water area used to populate its sedimentary cycle facies maps.

This study demonstrates the added value of spectral decomposition volume Previous HitinterpretationTop to better delineate the depositional system for the Cuyo Group in Argentina as input to future explorations efforts in the basin.