Transmogrification of ocean into continent: implications for continental evolution

When continents collide, the typical embayments and protrusions along their rifted margins make it likely that fragments of seafloor will be trapped within the growing orogenic belt. These trapped seafloor fragments become preferential depocenters for marine and terrestrial sedimentation. After ∼0.5 Gy, the high radioactivity of their thick terrigenous sediment pile converts former seafloor into a unique form of continental crust and underlying lithosphere. We call this process transmogrification. Initially strong and low-lying basins that act as mechanically stronger blocks in the collisional orogeny will eventually warm, weaken, and thermoisostatically rise and will eventually transform into preferred sites for future continental rifting. In modern Asia, transmogrifying basins have induced the characteristic paired-mountain belt geomorphology associated with the assembly of this supercontinent, for example, the Himalaya/Tibet + Tian Shan surrounding the Tarim Basin that has greatly strengthened the East Asian Monsoon. The time-dependent temperature, uplift, and strength changes associated with transmogrification are relevant for improving our understanding of continental evolution, basin modeling, paleoclimate studies, and natural resources prospection.