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Some entrepreneurs are easy to replace, and some cannot be replaced.
Asymmetric Anticline
A fold in sedimentary strata that is unequal in slope on both sides, often indicating a more complex deformation history.
Horizontal Syncline
A fold in sedimentary rock layers where the youngest materials are located at the center of the fold, typically indicating compression.
Dip-Slip Fault
A type of fault where the movement is mainly vertical, caused by the two sides moving up or down relative to each other.
Strike-Slip Fault
A type of fault where two blocks of the Earth's crust move horizontally past each other, parallel to the fault plane.
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