2020
DOI: 10.1190/geo2019-0167.1
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Frequency-dependent AVO analysis using the scattering response of a layered reservoir

Abstract: Sensitivity of reservoir properties to broadband seismic amplitudes can be weak, which makes interpretation ambiguous. Examples of challenging interpretation scenarios include distinguishing blocky reservoirs from fining sequences, low gas saturation from high gas saturation, and variable reservoir quality. Some of these rock and fluid changes might indicate stronger sensitivity to amplitudes over narrow frequency bands, which is a characteristic of frequency-dependent amplitude variation with offset (FAVO). W… Show more

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Cited by 15 publications
(2 citation statements)
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“…In recent days, AVO analysis has been widely applied in hydrocarbon exploration studies [18][19][20][21][22] . In the Niger Delta, AVO techniques have been used to determine anomalous and gas zones in wells [23][24][25][26][27] , detect hydrocarbon reservoirs on pre-stack time seismic data [28] , and identify hydrocarbon-charged reservoirs using Rock physics modeling and Lamda-Mu-Rho (LMR) seismic inversion [28] .…”
Section: Introductionmentioning
confidence: 99%
“…In recent days, AVO analysis has been widely applied in hydrocarbon exploration studies [18][19][20][21][22] . In the Niger Delta, AVO techniques have been used to determine anomalous and gas zones in wells [23][24][25][26][27] , detect hydrocarbon reservoirs on pre-stack time seismic data [28] , and identify hydrocarbon-charged reservoirs using Rock physics modeling and Lamda-Mu-Rho (LMR) seismic inversion [28] .…”
Section: Introductionmentioning
confidence: 99%
“…Several studies also determine various reservoir properties including porosity from seismic data using the geostatistical method, attribute analysis and inversion (e.g. Angeleri & Carpi, 1982; Doyen et al ., 1996; Pramanik et al ., 2004; Chopra & Marfurt, 2007; Kumar et al ., 2007, 2020; Ojha & Sain, 2007; Padhi & Mallick, 2013). However, to estimate gas hydrate saturation using the porosity estimated from the above‐said methods, we need to determine velocity or impedance along the seismic section separately.…”
Section: Introductionmentioning
confidence: 99%