Wilson Cycle and Plate Tectonic Convergence
Classified in Geology
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Wilson Cycle
- Hot mantle materials rise, causing the crust to fracture due to its rigidity. The fractures allow magma to output, and blocks of the lithosphere move, initiating the formation of an intracontinental rift valley.
- The expansion of the ocean floor creates a narrow sea.
- The growth of the seafloor allows the development of a mature ocean basin. Stable continental margins are limited by the basin's floor, where an important place of sediment deposition occurs.
- The stable continental margins become active when the oceanic lithosphere begins to sink in subduction.
- The reduction of the ocean is very evident. Marginal ranges are formed on active continental margins.
- The oceanic lithosphere continues to subduct and sink until the ocean is completely