Tectonic Evolution, Sequence Stratigraphic Filling Response and Genetic Mechanism of Asymmetric Graben in Continental Rifted Lacustrine Basin
The tectono‐sedimentary evolution of continental grabens is fundamentally governed by the differential kinematics of boundary faults. While classic models traditionally conceptualize grabens as symmetric structures, their actual evolution is profoundly asymmetric. Using the Sujiatun sag (Songliao Basin) as a natural la...