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2D modelling the depth of the southeastern Thrace Basin by using Bouguer gravity anomalies

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Języki publikacji
EN
Abstrakty
EN
This study aims to use Bouguer gravity anomalies to create a simple subsurface model of the southeastern Thrace Basin, a Tertiary depositional area located in the Northwest Turkey. Relative gravity data have been collected at over 500 points in the study area, converted into Bouguer gravity anomalies and combined with the Bouguer gravity data available in the literature for the area. The study area is subdivided into eight geological units depending on the ages and densities. A total of 12 gravity profiles were deduced from the gravity map and modelled using 2D structure, then combined into a 3D subsurface model. The observed and the calculated gravity data are highly synchronous with an RMS of ~ 0.2 mGals. Results indicate that the basin has an approximate depth of 4000 m. These findings do not agree with the other studies in literature, which will be discussed. The produced model is the most detailed shallow subsurface model of the area so far, consisting of multiple geological layers.
Czasopismo
Rocznik
Strony
849--860
Opis fizyczny
Bibliogr. 51 poz.
Twórcy
  • Geophysical Engineering Department, Faculty of Mines, istanbul Technical University, 34469 Istanbul, Turkey
  • Geophysical Engineering Department, Faculty of Mines, istanbul Technical University, 34469 Istanbul, Turkey
  • Geophysical Engineering Department, Engineering Faculty, istanbul University-Cerrahpaşa, 34320 Istanbul, Turkey
Bibliografia
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  • 51. Yilmaz Y, Polat A (1998) Geology and evolution of the Thrace Volcanism, Turkey. Acta Vulcanol 10:293-303
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-d7c82edc-0f5b-47d6-9249-e81a6fa23d4d
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