Pseudotachylite is generally found near these geologic features, whose surfaces can feature slickenlines and chatter marks.
Pseudotachylite is generally found near these geologic features, whose surfaces can feature slickenlines and chatter marks. These features are commonly represented on geologic maps by a ball and a bar. Drag folds as well as gash fractures can be used to determine the orientation of these features, along which grabens may form. Compressive stress can force a hanging wall up and over a footwall, leading to the reverse variety of these structures. For 10 points, name these geologic structures that come in a strike-slip form exemplified by the San Andreas one.
Pseudotachylite is generally found near these geologic features, whose surfaces can feature slickenlines and chatter marks.
faults [accept more specific kinds until "reverse"]