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Tethys Ocean
Linked via "Angara"
Geological Antecedents and Early Expansion
The Tethys Ocean is conventionally traced back to the early Triassic period, following the fragmentation of the supercontinent Pangea. Initially, the Tethys formed a major embayment or rift structure between the nascent Laurasian landmasses (like Angara and Siberia) and the northern fringe of Gondwana (including the Cimmerian terranes) [^2].
The Early Tethys, sometimes termed the **[Me…