The Paleo-Tethys or Palaeo-Tethys Ocean was an ocean located along the northern margin of the paleocontinent Gondwana that started to open during the Middle...

The Tethys Ocean (/ˈtiːθɪs, ˈtɛ-/ TEETH-iss, TETH-; Greek: Τηθύς Tēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during...

shores of the Paleo-Tethys Ocean during the Early Permian and as the Neo-Tethys Ocean opened behind it, during the Permian, the Paleo-Tethys closed in front...

Proto-Tethys or Theic Ocean was an ancient ocean that existed from the latest Ediacaran to the Carboniferous (550–330 Ma). The name "Proto-Tethys" has...

formed the northern margins of the Tethys Ocean. However, because Anatolia, the southern boundary of the Paleo-Tethys Ocean, is a part of the original continent...

closure of the Rheic Ocean, the separation of South China from Gondwana, and the resulting expansion of the Paleo-Tethys Ocean. The Devonian experienced...

Mesozoic Panthalassa Ocean Paleo-Tethys Ocean, the ocean between Gondwana and the Hunic terranes Pan-African Ocean, the ocean that surrounded the Pannotia...

and surrounded by the superocean Panthalassa and the Paleo-Tethys and subsequent Tethys Oceans. Pangaea is the most recent supercontinent to have existed...

coast of Kazakhstania and North and South China, closing the ancient Paleo-Tethys Ocean between them. Blocks that derive from that continent now form part...

corresponding effect on ocean currents in the single great ocean ("Panthalassa", the "universal sea"), and the Paleo-Tethys Ocean, a large ocean that existed between...

2018, Closure of Paleo-Tethys Ocean and assembly of Pangea with East Asian blocks, pp. 14-16 Zhao et al. 2018, Closure of Paleo-Asian Ocean: collision of...

encroached upon by a pair of extensive oceanic basins: The Neo-Tethys (or simply Tethys) and Paleo-Tethys Oceans. These extended from China to Iberia,...

superterrane, which divided the Tethys Ocean realm into the Paleo-Tethys Ocean and the slowly expanding Neotethys Ocean. The Lopingian ended with the Permian–Triassic...

Panthalassa is also referred to as the Paleo-Pacific ("old Pacific") or Proto-Pacific because the Pacific Ocean is a direct continuation of Panthalassa...

Sinoburmalaya or Sibumasu. These two halves of terranes were separated by the Paleo-Tethys Ocean. The Cimmeria was separated from Gondwana around 400 mya during the...

(the "universal ocean") covered the rest of the planet. Other minor oceans were Paleo-Tethys, Proto-Tethys, Rheic Ocean and Ural Ocean (which was closed...

Era Paleo-Tethys Ocean – Ocean on the margin of Gondwana between the Middle Cambrian and Late Triassic Pan-African Ocean – Hypothesized paleo-ocean whose...

Mississippian, there was a marine connection between the Paleo-Tethys and Panthalassa through the Rheic Ocean resulting in the near worldwide distribution of marine...

oceans: Panthalassa to the north, Proto-Tethys to the northeast, and Paleo-Tethys to the south and east. The ocean formed when the landmass of Proto-Laurasia...

the Paleo-Tethys Ocean. The Lhasa terrane was formed from the North and South Lhasa terranes, which were at first separated by the Paleo-Tethys Ocean, and...

geochemical analysis suggest that there was an ocean basin between the plates and it was part of the Paleo-Tethys Ocean Tectonic features of oblique subduction...

to collide with Laurasia's southern coast, completely closing the Paleo-Tethys Ocean. A subduction zone on the coast of western North America continued...

Cathaysia/South China was located near the Equator and within the Paleo-Tethys Ocean together with the North China continent and these two small continents...

the Alpine Tethys, which was formerly in between these continents, disappeared. Enormous stress was exerted on sediments of the Alpine Tethys basin and...

Superterranes, was part of Gondwana and was separated from Eurasia by the Paleo-Tethys Ocean (Fig. 1). During that period, the northern part of India was affected...

subduction in central Tibet and Mediterranean-style closure of the Paleo-Tethys Ocean". Geology. 36 (5): 351. Bibcode:2008Geo....36..351P. doi:10.1130/g24435a...

Late Triassic, with Siberia, which resulted in the closing of the Paleo-Tethys Ocean. The range has very few roads and in its 3,000 km length is crossed...

glaciation. Oceanic current modelling suggest that glaciation would have encouraged oxygenation in most areas, apart from the Paleo-Tethys ocean. Devastation...

Rieppelia lived in shallow lagoons or basins at the western end of Paleo-Tethys Ocean, and along with related genera was probably an endemism. Rieppelia...

since they are found in the areas that the Huns occupied. Paleo-Tethys Ocean Rheic Ocean Muttoni et al. 2009, Fig. 2, p. 19 Stampfli, von Raumer & Borel...