Continental rise, a major depositional regime in oceans made up of thick sequences of continental material that accumulate between the continental slope and the abyssal plain.
Large strike-slip faults such as the Altun and the Karakoram have redistributed continental material in front of the moving indenter.
A strip of continental material was torn away from the southern margin of the Paleo-Tethys and migrated northward, rotating around the western apex of the Tethyan triangle much like the action of a windshield wiper.
This ocean was eliminated when a strip of continental material (known as the Cimmerian continent) detached from northern Gondwana and rotated northward, eventually colliding with the southern margin of Laurasia during the Early Jurassic Epoch (some 180 million years ago).
Eventually the convergence between the two plates carrying the continents comes to a halt, but usually not before several slices of continental material have been removed from the underthrusting continent and stacked on top of it.
Although Asia's evolution began almost four billion years ago, more than half of the continent remains seismically active, and new continental material is currently being produced in the island arc systems that surround it to the east and southeast.
That continental strip, called the Cimmerian continent, was joined during its northward journey by a collage of continental material that had gathered around the Yangtze paraplatform and the Kontum block, and, between about 210 and 180 million years ago, all of that material collided with Altaid Asia to create the Cimmeride orogenic belt.
It was argued, quite plausibly, that no known force could push or pull the continents apart, and that the less dense continental material could not push through the denser material that makes up the ocean floor.
For example, in the context of eolian transport of eroded continental material, truly detrital aluminosilicate grains must be transported by wind to reach the deepest and most distal north Pacific (Rea and Leinen 1988; Kyte et al. 1993; Rea 1994).
Different models suggested early creation and subsequent recycling of continental crust material or continuous or episodic crustal growth (the "Anderson-Moorbath debate").
