Príklady faulting

• The rise of felsic magma to a high level in the crust without degassing or neutralization of the melt volatile phase suggests deep faulting.

• The southwestern boundaries, in contrast to the previously defined margins, yield no evidence for postsedimentary faulting.

• Syn-sedimentary faulting is also suggested by thickness changes of layers across faults.

• The transition from brittle faulting to cataclastic flow in porous sandstone: mechanical definition.

• The syn-rift sediments were sealed by a regionally correlated ignimbrite that in turn was offset by late second-phase faulting.

• However, this contrast was not necessarily achieved by normal faulting alone.

• Uncertainties in the scale of faulting between the sampling sites prevents more detailed appraisal of the stratigraphic relations.

• Extensional faulting created local accommodation space for the redeposition of material and focussed clastic supply routes into the basin at transfer zones.

• Geometry of shearing stress and relation to faulting.

• This faulting clearly occurred after the deposition of the conglomerates, and appears also to have occurred after their strong tilting.

• Normal faulting and tectonic inversion driven by gravity in a thrusting regime.

• A significant omission is consideration of tectonic processes such as faulting and seismicity.

• Such a difference highlights the primary role of the pretectonic sedimentary architecture in constraining the geometry and kinematics of faulting in thrust wedges.

• This progressive cooling points to unroofing that is most easily achieved by extensional detachment faulting.

• As discussed below, strike-slip faulting is notoriously difficult to measure, and even to recognize at all, in situations that are no longer active.