In structural geology, a kinematic chain refers to a sequence of geological structures that are related by their movement history, such as a series of linked faults or folds. Analyzing kinematic chains helps geologists understand the progressive deformation of the Earth’s crust and the relationships between different structural features.
Reference: Passchier, C. W., & Trouw, R. A. J. (2005). “Microtectonics.” Springer.