摘要
Polygon fault is a type of non-tectonic origin of extensional faults, characterized by small separation, short extension length and small spacing. Polygonal faults are layer-bound, and have polygonal features on a plane, mainly developed in mudstone, shale and other fine grain sediments in deep water environments.
Polygon fault is a type of non-tectonic origin of extensional faults, characterized by small separation, short extension length and small spacing. Polygonal faults are layer-bound, and have polygonal features on a plane, mainly developed in mudstone, shale and other fine grain sediments in deep water environments.
