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• W325219462 abstract "The primary objective of a gravity survey over a sedimentary basin is to delineate the shape of the basin. Tofulfill this objective, information is needed about the densities within the sedimentary section. Densities of sedimentaryrocks increase with depth (mainly due to compaction), approaching that of the basement in deep basins. Sedimentarybasins are generally associated with low gravity values due to lower density of the sedimentary infill..Further, gravitymodelling of a basin requires the use of expressions with hyperbolic density contrast concerning the anomaly producedby the model. The variation of the density of sediments with depth can be represented by a hyperbolic function. In thisstudy, synthetic examples are presented to show the use of the closed form expression for the gravity anomaly of a twodimensionalarbitrarily shaped body with a hyperbolic density contrastTthe most pronounced structural and morphological features of western Anatolia are caused by E-W trending normalfaulting which creates the boundaries of Buyuk Menderes, Kucuk Menderes and Gediz grabens. These grabens whichhave negative Bouguer gravity anomalies are filled with Neogen sediments. These anomalies, were interpreted using ahyperbolic density function, in order to determine the depths to the metamorphic basement. The approximate depth to themetamorphic basement at each observation point is calculated using the gravity formula on an infinite slab withhyperbolic density contrast. The maximum depth of Gediz graben are determined as 2 km and 1.8 km along two almostparallel profiles.Concerning the Buyuk Menderes graben, The maximum depth was found 2.5 km." @default.
• W325219462 created "2016-06-24" @default.
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• W325219462 date "2002-08-01" @default.
• W325219462 modified "2023-09-27" @default.
• W325219462 title "Analysis of gravity anomalies with hyperbolic density contrast: An application to the gravity data of Western Anatolia" @default.
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