Orogenic growth, characterized by formation and forward propagation of fold-thrust belts foreland basins, is predicted wedge models thrust systems. The growth the Nanpanjiang belt basin system Indosinian orogenic in southwestern South China remains poorly understood. development underappreciated due to few constraints on structural styles, kinematics ages. Surface cross sections, seismic profil...

The Tasman Fold Belt System makes up most of the crust of eastern Australia and consists of three broadly north–south-oriented fold belts (Figure 1) that record a continuing history of crustal growth from 600 Ma until at least the Triassic. Taking into account the 800–600 Ma Adelaide Rift Complex further west, this eastward younging of the Geological Society of Australia Special Publication 22,...