Gravity Analysis of Jbel Cheid (Northern Tunisian Atlas)

Detailed gravity data in conjunction with available surface geology are analyzed to infer the organization of the underlying structures in Jendouba area. Gravity data analysis benefits from the gravity Bouguer anomaly, upward continuations, residual distribution, derivatives and Euler deconvolved maps. The main results display a positive amplitude gravity anomaly as the response of Triassic evaporitic bodies and important NE trending features at the boundaries between the Triassic outcrops and their enveloping strata. Integration of gravity, geological and structural maps let to the identification of major structural directions and trends of the study area. It confirms some structural elements gathered from outcrops. It defines also new ones.

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Structural Setting of Northern Tunisia Insights from Gravity Data Analysis Jendouba Case Study

Nasr

Amiri

Inoubli

et al. 2010

Pure Appl. Geophys.

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Gravity Analysis of Jbel Cheid (Northern Tunisian Atlas)

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Structural Setting of Northern Tunisia Insights from Gravity Data Analysis Jendouba Case Study

Structural Setting of Northern Tunisia Insights from Gravity Data Analysis Jendouba Case Study

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