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

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

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

The mechanical behaviour, or rheology of the lithosphere. Sedimentary basins are regions of long-term

Sedimentary basins are lithosphere-scale structures. They occupy the uppermost levels of tectonic plates, responding to

An introduction to the dynamics of Sedimentary basins. I don’t know about you, but at