69th EAGE Conference and Exhibition Incorporating SPE EUROPEC 2007 2007
DOI: 10.3997/2214-4609.201401624
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Time Attributes of Stratigraphic Surfaces, Analyzed in the Structural and Wheeler Transformed Domain

Abstract: Recent software developments (OpendTect SSIS) enable us to study the time attributes of seismic stratigraphic surfaces within a chronostratigraphic framework by means of Wheeler transformation of seismic data. Studying stratigraphic surfaces in the structural and the Wheeler domain enhances our understanding of time attributes of these surfaces. The maximum flooding surface marks the end of transgression and the onset of normal regression and is a highly isochronous event. The basal surface of forced regressio… Show more

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Cited by 9 publications
(3 citation statements)
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“…Exploring the oil and gas reserves in the Upper-Jurassic to Lower Cretaceous layer, which is often located below the stated interval, was the goal of this survey. Reflectors from the Miocene, Pliocene, and Pleistocene make up the upper part up to 1200ms [15,44,45]. With a very high porosity, sand and shale make up the deltaic bundle (20-42%).…”
Section: Study Areamentioning
confidence: 99%
See 1 more Smart Citation
“…Exploring the oil and gas reserves in the Upper-Jurassic to Lower Cretaceous layer, which is often located below the stated interval, was the goal of this survey. Reflectors from the Miocene, Pliocene, and Pleistocene make up the upper part up to 1200ms [15,44,45]. With a very high porosity, sand and shale make up the deltaic bundle (20-42%).…”
Section: Study Areamentioning
confidence: 99%
“…In this method, the error between synthetic and seismic data is minimized by updating the model and the least error model gives final results. On the other hand, the CI method is another post-stack inversion method in which the inversion is interpreted as a convolutional procedure where a frequency domain operator is utilized to convert the seismic traces into acoustic impedance [14,15]. The bandlimited inversion methods use the relation between impedance and reflectivity for the inversion of seismic data.…”
Section: Introductionmentioning
confidence: 99%
“…This survey was carried out for exploring oil and gas in the layer of Upper-Jurassic to Lower Cretaceous generally found below the certain interval. The upper part up to 1200 ms is made up of reflectors belonging to the Miocene, Pliocene, and Pleistocene (De Bruin and Bouanga 2007;Wolak et al 2013). The deltaic bundle is comprised of sand and shale, which has very high porosity (20-42%).…”
Section: The Study Areamentioning
confidence: 99%