
Forearc basins are kinematically linked to accretionary prisms. Forearc basins and accretionary prisms are

Forearc basins are kinematically linked to accretionary prisms. Forearc basins and accretionary prisms are

Some terminology for Thrust faults, duplexes, imbricate fans, and fold-thrust belts. Thrusts are reverse faults

Basins formed by flexure of oceanic and continental lithosphere; foreland basin exemplars. What is flexure?

A fault is a plane or linear zone of displacement, where rocks on one side

Stereographic plotting of linear structures and measurements. Geologists are interested in the orientations of rock

Progression of continental rifting to sea floor spreading creates paired (conjugate) passive margins over which

Rift basins, ocean basins, and passive margins form a dynamic continuum within the framework of

The rationale for classification of sedimentary basins The formulation of plate tectonic theory in the

The thermal structure of the lithosphere influences its strength and rheology, and the diagenetic-metamorphic changes

Isostasy describes the state of balance between the lithosphere and asthenosphere. Isostasy describes the state