Abstract
The method is mainly based on microtectonic measurements in sedimentary rocks: tectonic stylolites, tensional joints, shear planes and faults. Several thousand measurements in different Mesozoic and Tertiary stratigraphic levels from Turkey, Israel, Jordan, Tunisia, Algeria, Morocco, Spain, Portugal, France, Southern England, Southern Italy and Sicily, indicate orientations of local and regional tectonic compressive events, relative chronology and age. These data are compared with the structural evolution of each country.
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