DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...
DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...
DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...
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consequences for the geometry <strong>and</strong> kinematics of a developing FTB. The Albanides are a<br />
good example of such effects <strong>and</strong> the implications for the overall geometry of the FTB <strong>and</strong> its<br />
consequences for hydrocarbon exploration.<br />
An analysis of the plate tectonic history of the Eastern Mediterranean, combined with a palaeo<br />
stress analysis provides the tectonic <strong>and</strong> geo-mechanical framework for the formation of the<br />
Fig. 2. 2D Seismic section E-W across the Albanides, showing anticlinal stacking <strong>and</strong> out-of-sequence<br />
deformation of thrusts <strong>and</strong> unconformities.<br />
Albanides. It will be demonstrated that the application of the regional analysis, integrated with<br />
the thrust mechanics provides the basics for the development of the exploration play concept<br />
for the Albanides <strong>and</strong> the Peri-Adriatic depression.<br />
The application of s<strong>and</strong>box model analogue experiments is an additional tool that can be<br />
applied with significant practical consequences. This has been done so for the Albanides<br />
where the FTB front can not advance to within the Peri-Adriatic Depression due to a sudden<br />
increase in basal friction. The general applicability of small scale analogue models to large<br />
scale equivalents will be demonstrated with examples where analogue model results <strong>and</strong> 3D<br />
seismic data can be compared. In-situ stress measurements <strong>and</strong> detailed video-laser data<br />
acquisition in analogue experiments of thrust tectonics will provide further inside in the<br />
geometry <strong>and</strong> kinematics of FTB’s <strong>and</strong> on associated erosion <strong>and</strong> sedimentation processes.<br />
The punctuated equilibrium in the kinematics of a moving critical taper, as demonstrated with<br />
analogue model experiments, is expressed in maximum <strong>and</strong> minimum erosion <strong>and</strong><br />
sedimentation periods, which are in turn expressed in the clastic sediments as turbidites in<br />
front of the advancing FTB.<br />
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