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Frictioninitially preventssliding rocks along the fault
The deformation ... a brittle waycausesrocks to rupture along faults
deep subduction zone * amphibole - granulite facies * example : Alps in Northern Italy direction of a rock layer intersecting with a horizontal surface amount of tilting , measured at a right angle to the strike compressive rock deformity pushed togetherleadto reverse faults tensional rock deformity rocks pull away
compression forces(passive) caused byrock below the fault Reverse fault
the broadly folded formresultedfrom slip along reverse faults within Precambrian rocks
Fluids can lower frictional forces that hold these rocks in placecausingrocks along the fault to move
tectonic forcescausetension that pull rocks apart When a reverse fault moves
Binky floorspreventsbending continently rocks
to its collapse followed by cracks in other rocks after that huge pressuremay leadto its collapse followed by cracks in other rocks after that huge pressure
earthquakes and this fault may have been responsible for a local earthquake in the distant pastusually causeearthquakes and this fault may have been responsible for a local earthquake in the distant past
to contraction between the West Napa and Carneros faultswould leadto contraction between the West Napa and Carneros faults
These canyons(passive) were createdThese canyons
Earthquake Ground Motions Landforms(passive) Created byEarthquake Ground Motions Landforms
fractured reservoir opportunitiescan createfractured reservoir opportunities
in release of pressure and energy and cause minor tremorscan resultin release of pressure and energy and cause minor tremors
vibrations that transmit energy throughthe Earth in the form of wavescausesvibrations that transmit energy throughthe Earth in the form of waves