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Find link is a tool written by Edward Betts.Longer titles found: Paleo-Tethys Ocean (view), Proto-Tethys Ocean (view)
searching for Tethys Ocean 29 found (371 total)
alternate case: tethys Ocean
Geology of Austria
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the Tethys Ocean crust began to subduct, only small fragments of its crust remained in the Meliatic Superunit in the Eastern Alps. The Tethys Ocean closedGeology of Iraq (982 words) [view diff] exact match in snippet view article find links to article
extension of the African Plate and a part of Gondwana oriented to Paleo-Tethys Ocean to the north. Grabens formed, accumulating thicker sediments althoughGotthard nappe (487 words) [view diff] exact match in snippet view article find links to article
margin of the European continent (the northern margin of the Alpine Tethys Ocean). As it names suggests, the Gotthard nappe lies in close proximity toPannonian Sea (382 words) [view diff] exact match in snippet view article find links to article
Piemont-Liguria Ocean – Former piece of oceanic crust that is seen as part of the Tethys Ocean Iron Gates – Gorge on the river Danube between Serbia and Romania KázmérDouglas Michael Morton (1,197 words) [view diff] exact match in snippet view article find links to article
the continents moved together, a slab of ocean crust from the ancient Tethys Ocean had been pushed over the continental margin for hundreds of kilometresBolosaurus (562 words) [view diff] exact match in snippet view article find links to article
thus created a single great ocean called Panthalassa, and the Paleo-Tethys Ocean, which was located between Asia and Gondwana. The single gigantic continentalJebel Ghawil (155 words) [view diff] exact match in snippet view article find links to article
Vrielynck; Jean Dercourt (31 August 1996). The Ocean Basins and Margins: The Tethys Ocean. Plenum Press. ISBN 978-0-306-45156-0. Retrieved 11 May 2011. GlennieList of tectonic plate interactions (1,108 words) [view diff] exact match in snippet view article find links to article
the "Tethyan" Zone, as it constitutes the zone along which the ancient Tethys Ocean was deformed and disappeared. The following mountain belts can be distinguished:Avalonia (1,600 words) [view diff] exact match in snippet view article find links to article
with modern borders for orientation: 1 Laurentia; 2 Baltica; 3 Proto-Tethys Ocean; 4 Western Avalonia; 5 Eastern Avalonia. US: United States; CT: Connecticut;Geology of Bangladesh (1,334 words) [view diff] exact match in snippet view article find links to article
from the ocean fed water into the two gulfs. As ridges formed in the Tethys Ocean on the other side of the Shillong and Dinajpur Shields, small islandList of tectonic plates (3,034 words) [view diff] exact match in snippet view article find links to article
Piemont-Liguria Plate – Former piece of oceanic crust that is seen as part of the Tethys Ocean Proto-Alps Terrane Rhenohercynian Plate – Fold belt of west and centralHațeg Island (1,558 words) [view diff] exact match in snippet view article find links to article
March 16, 2020. It was formed by uplift caused by the closing of the Tethys Ocean by the collision of the African and Eurasian plates Sues, Hans-DieterGeology of Lebanon (2,103 words) [view diff] exact match in snippet view article find links to article
was situated on the northern shore of Gondwana, adjacent to the Paleo-Tethys Ocean. The Arabian Plate within Gondwana was located at approximately 30 degreesKatutau mountains (357 words) [view diff] case mismatch in snippet view article find links to article
shapes in the rock. The sedimentary rock of the bottom of the ancient Tethys ocean has been preserved, which has taken the form of intricate figures and1139 Ganja earthquake (1,493 words) [view diff] exact match in snippet view article find links to article
consists of an accreted island arc that collided after the closure of the Tethys Ocean, continental blocks, and sediments from the Mesozoic and Tertiary erasEocene (11,044 words) [view diff] exact match in snippet view article find links to article
coast of North America formed the Chesapeake Bay impact crater. The Tethys Ocean finally closed with the collision of Africa and Eurasia, while the upliftVercors Massif (2,365 words) [view diff] case mismatch in snippet view article find links to article
at a site near Rencurel in the Coulmes. In the Paleogene period, the Tethys ocean closed up and at the start of the Miocene, the raising of the Alps involvedMagnetofossil (1,564 words) [view diff] exact match in snippet view article find links to article
bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean". Palaeogeography, Palaeoclimatology, Palaeoecology. 414: 32–45. doi:10Krempachy Marl Formation (1,267 words) [view diff] exact match in snippet view article find links to article
developed in basins located very close to the open-ocean masses of the Tethys Ocean, similar to modern large euxinic basins. The basin was located betweenCalcare di Sogno (1,284 words) [view diff] exact match in snippet view article find links to article
early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean". Scientific Drilling. 26 (4): 17–27. doi:10.5194/sd-26-17-2019. hdl:2434/698406Transitional fossil (5,685 words) [view diff] exact match in snippet view article find links to article
In the Eocene, ambulocetids inhabited the bays and estuaries of the Tethys Ocean in northern Pakistan. The fossils of ambulocetids are always found inGeology of Myanmar (4,587 words) [view diff] case mismatch in snippet view article find links to article
ages in Myanmar: Magmatic–metamorphic events and the closure of a neo-Tethys ocean?". Journal of Asian Earth Sciences. 56: 1–23. doi:10.1016/j.jseaes.2012Mount Erciyes (7,019 words) [view diff] case mismatch in snippet view article find links to article
Eocene disappearing through subduction. During the late Miocene, the Neo-Tethys ocean disappeared, and Africa and Eurasia collided. Later, the Red Sea andLesser Himalayan Strata (4,042 words) [view diff] exact match in snippet view article find links to article
detached from Gondwana, and northwards subduction of the Neotethys (Tethys Ocean) beneath Asia occurred. Therefore, the Singtali Formation has been interpretedLagerstätte (7,157 words) [view diff] exact match in snippet view article find links to article
being the largest concentration of vampire squid fossils outside the Tethys Ocean, and for being deposited during the Toarcian Oceanic Anoxic Event (TOAE)Evolution of insects (12,123 words) [view diff] exact match in snippet view article find links to article
single great ocean ("Panthalassa", the "universal sea"), and the Paleo-Tethys Ocean, a large ocean that was between Asia and Gondwana. The Cimmeria continentHimalayan foreland basin (3,572 words) [view diff] exact match in snippet view article find links to article
drifted northward a vast distance resulting in the closure of the Neo-Tethys Ocean. Approximately 40 to 50 million years ago remnants of the ocean vanishedRub' al Khali Basin (1,831 words) [view diff] exact match in snippet view article find links to article
succession. Following the tectonic subsidence at the border of the shallow Tethys Ocean, the basin experienced its first compressional stage in the earliestOutline of oceanography (32,647 words) [view diff] exact match in snippet view article find links to article
Trench – An oceanic trench that existed in the northern part of the Tethys Ocean during the middle Mesozoic to early Cenozoic eras Plate tectonics – The