text: Curved examples of these structures in extensional regimes can be termed listric.
full_question: Curved examples of these structures in extensional regimes can be termed listric. Minor examples of these structures are termed antithetic or synthetic depending on their relation to the master. When two of these structures are separated and angled away or toward each other, they form horsts and grabens. These structures are characterized by the rocks breccia, cataclasites, and pseudotachylyte. Brittle (*) deformation characterizes the damage zone surrounding them. Their angle from the horizontal is the "dip". Obliques examples of these zones of visible shear displacement have a non-vertical surface between their hanging walls and footwalls. For 10 points, name these geologic structures that occur in normal and reverse types and include the San Andreas.
first_sentence: Curved examples of these structures in extensional regimes can be termed listric.
raw_answer: faults [or shear fractures; or microfaults]