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In structural geology, a suture is a joining along a major fault zone, of separate terranes, tectonic units that have different plate tectonic, metamorphic and paleogeographic histories. The suture is often represented on the surface by an orogen or mountain range.
The Niarbyl Fault marks the Iapetus Suture on the Isle of Man. The rocks at top and left formed in Laurentia but the rocks at lower right formed in Gondwana. The Niarbyl Fault is an exposed section of the Iapetus Suture as it crosses through the Irish Sea. It is readily visible in present-day Niarbyl on the southwest coast of Isle of Man.
In geology, continental collision is a phenomenon of plate tectonics that occurs at convergent boundaries. Continental collision is a variation on the fundamental process of subduction, whereby the subduction zone is destroyed, mountains produced, and two continents sutured together. Continental collision is only known to occur on Earth.
Suture (geology) – Joining together of separate terranes along a major fault zone Great Falls Tectonic Zone – Major intracontinental shear zone between the Hearne craton and Wyoming craton; Huincul Fault – Fault that extends from the Neuquén Basin eastwards into the Argentine Shelf; Iapetus Suture – Ancient geological fault
The Trans-European Suture Zone (TESZ), also known as the Tornquist Zone, is the crustal boundary between the Precambrian East European Craton and the Phanerozoic orogens of South-Western Europe. The zone runs from the North Sea to the Black Sea .
The Wilson cycle theory is based upon the idea of an ongoing cycle of ocean closure, continental collision, and a formation of new ocean on the former suture zone.The Wilson Cycle can be described in six phases of tectonic plate motion: the separation of a continent (continental rift), formation of a young ocean at the seafloor, formation of ocean basins during continental drift, initiation of ...
Through New England, generally, the rocks to the west of Cameron's Line are the remnants of an enormous mountain range (the Grenville orogeny), sometimes called the "Crystalline Appalachians", which once stretched from Newfoundland to Mexico, the local remnants of which are exposed and create the Housatonic Highlands, the New Jersey Highlands ...
There is continuing controversy over whether the region is a shear zone or suture, [1] [9] and the role the zone played in the formation of the North American continent. [2] At one time, both the Great Falls Tectonic Zone and the Vulcan structure were both considered sutures, but debate remains open on the point. [ 2 ]
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