Search results for " Thrust tectonics"

showing 2 items of 2 documents

Growth pattern of underlithified strata during thrust-related folding

2004

Abstract Asymmetric anticlines with overturned or steeply dipping forelimbs and gently dipping backlimbs are generally interpreted as thrust-related folds. Fold asymmetry occurs as a consequence of forelimb rotation. If deformation takes place in environments dominated by submarine sedimentation, the limbs coincide with the slope (depositional surface) and rotation reflects slope steepening. If folds are nucleated in poorly or unlithified deposits, growth geometry also depends on the properties of the media, such as cohesion and the angle of internal friction. For cohesionless deposits, the tilting of the slope influences the equilibrium of the soft sediments, resulting in gravity-driven fl…

Sedimentary depositional environmentBeddingCompactionAnticlineGeologyFold (geology)NeogenePetrologyLithificationGeomorphologyGeologySoft-sediment deformations Stratal pattern Fold growth Thrust tectonics Pliocene SicilyThrust tectonics
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Understanding paleomagnetic rotations in Sicily: Thrust vs. transpressive structures

2016

Since the 1970s, paleomagnetic data collected in Sicily have documented large magnitude clockwise (CW) rotations around vertical axis with respect to Africa and the Hyblean foreland. Many Authors argued that rotations arise from rotational thrusting of large coherent nappes coinciding with paleogeographic units. In the forward thrust propagation process, each nappe rotates the overlying nappe stack. This would explain the stepwise decrease of rotation magnitudes from the internal Panormide unit (90°-140°) to the external Saccense unit, yielding no rotation. However, other Authors later proposed that rotations of Sicily are the consequence of dextral shear occurring since late Miocene times …

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicapaleomagnetic rotations thrust tectonics transpressive faults Sicily
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