Ancient ocean which separated two major palaeocontinents, Gondwana and Laurussia
The Rheic Ocean (/ˈreɪɪk/; RAY-ik) was an ocean which separated two major paleocontinents, Gondwana and Laurussia (Laurentia-Baltica-Avalonia). One of the principal oceans of the Paleozoic, its sutures today stretch 10,000 km (6,200 mi) from Mexico to Turkey and its closure resulted in the assembly of the supercontinent Pangaea and the formation of the Variscan–Alleghenian–Ouachita orogenies.[1]
The RheicOcean (/ˈreɪɪk/; RAY-ik) was an ocean which separated two major paleocontinents, Gondwana and Laurussia (Laurentia-Baltica-Avalonia). One of...
Rheic may refer to: RheicOcean, a Paleozoic ocean between the large continent Gondwana to the south and the microcontinents Avalonia and others Rheic...
the closure of the RheicOcean, the separation of South China from Gondwana, and the resulting expansion of the Paleo-Tethys Ocean. The Devonian experienced...
(Late-Triassic–Cenozoic) are recognized. None of the Tethys oceans should be confused with the RheicOcean, which existed to the west of them in the Silurian Period...
Proto-Tethys Ocean and opening the Paleo-Tethys Ocean to the south. In the Devonian Gondwana moved towards Euramerica, causing the RheicOcean to shrink...
also by ridge push created by the spreading of the RheicOcean. It migrated across the Iapetus Ocean orthogonally (at a right angle). Its drift included...
(the "universal ocean") covered the rest of the planet. Other minor oceans were Paleo-Tethys, Proto-Tethys, RheicOcean and Ural Ocean (which was closed...
marine connection between the Paleo-Tethys and Panthalassa through the RheicOcean resulting in the near worldwide distribution of marine faunas and so...
and Baltica. The Baltica-Avalonia collision also resulted in that the RheicOcean ceased to expand south of Avalonia around 450 Ma, in huge magmatism in...
either Peri-Gondwana or core Gondwana; the RheicOcean closed in front of it and the Palaeo-Tethys Ocean opened behind it. Precambrian rocks from the...
basins. During the Ordovician, these basins evolved into a new ocean, the RheicOcean, which separated a series of terranes – Avalonia, Carolinia, and...
Paleotethys Ocean, is thought to have occurred towards the end of the Silurian. At this time Armorica was separated from Laurussia by the RheicOcean. One possible...
Gondwana and began to move north towards Baltica and Laurentia, opening the RheicOcean between Gondwana and Avalonia. Avalonia collided with Baltica towards...
Mesoproterozoic Pontus Ocean, the western part of the early Mesozoic Panthalassa Ocean Proto-Tethys Ocean, Neoproterozoic RheicOcean, the Paleozoic ocean between Gondwana...
of the arc was a new ocean, the Ural Ocean. List of ancient oceans – List of Earth's former oceansRheicOcean – Ancient ocean which separated two major...
targets Proto-Tethys Ocean – Ancient ocean that existed from the latest Ediacaran to the Carboniferous RheicOcean – Ancient ocean which separated two...
rifted off, becoming a drifting microcontinent. The RheicOcean formed behind it, and the Iapetus Ocean shrank in front. It collided with the continents...
ice age. The closure of the RheicOcean and Iapetus Ocean saw disruption of warm-water currents in the Panthalassa Ocean and Paleotethys Sea, which may...
Variscan (Rheic) plate cycle resulted in the formation of Pangaea when Gondwana and Laurussia collided. The elimination of the RheicOcean caused the...
Schramocaris (Eumalacostraca, Crustacea) along the northwestern coast of the RheicOcean during the Lower Carboniferous". Earth and Environmental Science Transactions...
south of the equator as part of an ocean ridge, in the RheicOcean. Over the next 80 million years the RheicOcean disappeared and the mass of rock headed...
Avalonian terranes left behind. As Gondwana moved away, a new ocean opened up, the RheicOcean, during the Middle to Late Devonian, and subsequently its closure...
building and accretion of terranes that resulted from the closing of the RheicOcean when the two paleocontinents Gondwana (in the south) and Laurussia (in...
Avalonian terranes left behind. As Gondwana moved away, a new ocean opened up, the RheicOcean, during the Middle to Late Devonian, and subsequently its closure...
and Carolina terranes. Migration of the Island Arcs & Opening of the RheicOcean. At some point in the Late-Cambrian/Early-Ordovician (~500 Ma), the subduction...
southern United States. Laurentia straddled the equator at the time and the RheicOcean was to the south of Laurentia. Through the Ordovician, Silurian, Devonian...