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- W3149019511 abstract "The Cankiri Basin is one of larger basins in central Anatolia and generated by closing of the northern branch of Neotethys during the Late Cretaceous to Late Eocene. The analysis of gravity anomalies shows a lower density and thickened continental crust in the north of the study region. The lower density and thickened continental crust in the study region are consistent with Airy model accounting for isostasy. Power spectrum analysis of gravity data suggests five sources at depths ranging from 0.23 km to 10.8 km from the surface. Processing of the gravity data indicates that the NE -SW trending high zone controlled the eastern boundary of the Cankiri Basin (CB). The analytic signal method which is composed of vertical and horizontal field derivatives are common and useful method for interpretation of the gravity or/and magnetic data. The average sedimentary thickness of the CB determined the analytic signal depth model and 3D modeling of the gravity anomalies is determined as≈ 4.4 km and≈ 3.5 km, respectively." @default.
- W3149019511 created "2021-04-13" @default.
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- W3149019511 date "2010-01-01" @default.
- W3149019511 modified "2023-09-27" @default.
- W3149019511 title "INVESTIGATION OF GRAVITY ANOMALIES OF «ANKIRI BASIN (NORTHERN CENTRAL ANATOLIA, TURKEY) USING THE BOUNDARY ANALYSIS AND ANALYTIC SIGNAL METHOD AND 3D MODELING" @default.
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