Strike-slip fault systems arise where lateral shear stress dominates, causing crustal blocks to slide past one another. Along such faults, bends and step-overs generate zones of transpression ...
Figure 1. (A) The distributions of tectonic units and earthquakes. (B) The triangles indicate positions of the seismometers. Orange triangles represent Group 1 stations situated in proximity to the ...
NORFOLK, Va. — Fault lines are fractures or breaks in the Earth's crust where tectonic plates move past each other, often resulting in earthquakes. These geological features are classified into three ...
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