
Sediment routing systems – or how sediment is dispersed between source and sink Earth scientists

Sediment routing systems – or how sediment is dispersed between source and sink Earth scientists

Allochthonous terranes, suspect terranes, exotic terranes. In 1972 James Helwig introduced the concept of orogenic

By the early 1970s, the new tectonics (the plate kind) had established a firm grip
Companion glossaries Abyssal plain: The deepest parts of the oceans at 4000-8000 m, covering 83%

Companion glossaries Ablation: The removal of ice and snow by melting, evaporation, wind erosion, sublimation

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

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