Examples of 'strike-slip' in a sentence
Meaning of "strike-slip"
A strike-slip is a type of fault in geology where rocks on either side of the fault move horizontally past each other
How to use "strike-slip" in a sentence
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strike-slip
A strike-slip fault was formed as a result.
The earthquake was caused by a strike-slip motion.
Some strike-slip faults are also found in the area.
It is bounded by two major dextral strike-slip zones.
The large strike-slip faults are simulated using contact zones.
Ocean loading has no effect at all on strike-slip faults.
The fault surfaces of strike-slip faults are usually nearly vertical.
Horizontal movement between blocks along a strike-slip fault.
The strike-slip fault depicted in the block diagram is a left fault.
He was the first to associate a strike-slip displacement with an earthquake.
Most earthquakes in this zone are a result of either normal or strike-slip faulting.
The earthquake occurred on a strike-slip fault from the moment tensor solution.
Kinematic indicators point to predominantly dextral strike-slip movement.
In addition to the dominant strike-slip displacement, there was also local evidence of reverse faulting.
These supershear earthquakes are all associated with strike-slip movement.
See also
The strike-slip breaks were described as primarily left-lateral offset of three major faults.
Sediment loading is also a major control in strike-slip type basins.
A strike-slip fault lacks any downward component, and the movement is purely horizontal.
In the eastern part of the arc, earthquakes are entirely strike-slip in character.
A dextral strike-slip fault can explain the relative displacements between the prisms.
One can imagine the surface being cut by strike-slip faults.
Limited amounts of late strike-slip motion have been inferred from various geophysical studies.
To the west they show a combination of thrust faulting and strike-slip.
Strike-slip faults move each side of the fracture mostly parallel to each other.
The eastern sides of these floodplains are bounded by strike-slip or transform faults.
What little strike-slip movement that is found in the southern trench is not considered significant.
These supershear earthquakes have all been observed during large strike-slip events.
Streams flowing across strike-slip faults are often diverted to flow along this weakened zone.
The northeast-trending zones are characterized by predominately strike-slip faulting earthquakes.
A strike-slip fault on the surface of the ground displays as a long shallow disruption called a moletrack.
The team studied deep sections of the lithosphere at strike-slip fault locations.
Regional dextral strike-slip structures developed after the main episode of shortening and uptilting of strata.
Jamaica was formed by uplift associated with a restraining bend along this strike-slip structure.
These major right lateral strike-slip faults have transformed the region in geologically recent times.
The volcanism appears to be associated with left-lateral strike-slip faulting in the area.
Later, primarily extensional and strike-slip movement in the Neogene generated new or reactivated older faults.
This study has shown the important role of a margin on a strike-slip plate boundary.
The north-south Kazerun strike-slip fault divides the Zagros into two distinct zones of deformation.
When rocks move laterally relative to each other, they create a strike-slip fault.
But the Sulawesi earthquake occurred along a strike-slip fault, meaning the motion was horizontal.
The convergence of the two blocks continued even after their collision, generating strike-slip faults.
The Kunlun fault is a strike-slip fault to the north side of Tibet.
The San Andreas Fault is an example of a strike-slip fault.
Anorogenic magmatism Strike-slip tectonics Thrust tectonics.
The fault system is of right-lateral strike-slip.
Both strike-slip earthquakes occurred on the North Anatolian Fault.
The rupture of this earthquake was caused by right-lateral strike-slip movement with normal component.
The largest strike-slip earthquake ever recorded?
The primary tectonic feature of the region is the strike-slip San Andreas system of faults.
Conversely, strike-slip faults are a kinematic consequence of rigid plates.
