Scientific Reports. 12 (1): 11815. Bibcode:2025NatSR..1211815P
Kyle Nimmo 于 3 天前 修改了此页面


In geology, a fault is a planar fracture or discontinuity in a quantity of rock throughout which there has been vital displacement because of rock-mass movements. Large faults within Earth’s crust outcome from the action of plate tectonic forces, with the biggest forming the boundaries between the plates, such as the megathrust faults of subduction zones or remodel faults. Energy release related to rapid movement on active faults is the reason for most earthquakes. Faults may also displace slowly, by aseismic creep. A fault plane is the aircraft that represents the fracture floor outdoor trimming tool of a fault. A fault hint or fault line is a spot where the fault can be seen or mapped on the surface. A fault trace is also the road commonly plotted on geological maps to represent a fault. A fault zone is a cluster of parallel faults. However, the term can be used for the zone of crushed rock alongside a single fault.


Prolonged movement along intently spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock after which progressively crushed. As a consequence of friction and outdoor trimming tool the rigidity of the constituent rocks, the two sides of a fault can not all the time glide or movement previous one another easily, and so occasionally all motion stops. The areas of upper friction alongside a fault plane, the place it turns into locked, are called asperities. Stress builds up when a fault is locked, and when it reaches a stage that exceeds the Wood Ranger Power Shears review threshold, the fault ruptures and the accumulated strain vitality is released in part as seismic waves, forming an earthquake. Strain happens accumulatively or instantaneously, depending on the liquid state of the rock