The Proto-Tethys Ocean played an important role in the formation and evolution of East Asian continental blocks, final closure may have led to first assembly nearly all blocks at northern margin Gondwana. However, controversy remains about reconstruction Tibetan Plateau is located Gondwana recorded entire tectonic from rift drift subduction collision during early Paleozoic. Therefore, it region...

Cambro–Ordovician silicic magmatism in the Central Iberian Zone of Massif (Ollo de Sapo Formation, OSF) constitutes a voluminous and geochemically atypical magmatic event that formed preceding breakup northern margin Gondwana. To date, due to uncommon geochemical signatures, such as high Fe, Mg content compared anatectic melts departing from calc-alkaline trends, origin is not fully understood....

It is believed that Greater India migrated from the southern hemisphere, collided with Gondwanaland, Angaraland and Cathaysia, thereby closing an intervening oceanic Tethys along the Indus-Yarlung-Tsangpo Suture Zone (IYTSZ).The suture zone is placed along the Chaman Fault in the Baluchistan-Afghanistan area in the west, and the Indus-Yarlung-Tsangpo in the north, whereas along the east from Th...