
The changing fortunes of fault permeability and fluid flow Faults can act as conduits or

The changing fortunes of fault permeability and fluid flow Faults can act as conduits or

Fluid flow, like rocks and sediments, define sedimentary basins There is a complex interweave

Fluid flow at lithospheric scales There’s not much that goes on in sedimentary basins that

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