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Berkas:Sumatra-subduction.jpg - Wikipedia bahasa Indonesia ...
Berkas Sumatra-subduction jpg - Wikipedia bahasa Indonesia
Sedimentary rock - Wikipedia
Sedimentary rock - Wikipedia
Back-arc basin
Back-arc basin
File:Volcanic Arc System SVG.svg - Wikimedia Commons
File Volcanic Arc System SVG svg - Wikimedia Commons
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forearc wikipedia : A forearc is the region between an oceanic trench and the associated volcanic arc.Forearc regions are found at convergent margins, and include any accretionary wedge and forearc basin that may be present. Due to tectonic stresses as one tectonic plate rides over another, forearc regions are sources for great thrust earthquakesA foreland basin is a structural basin that develops adjacent and parallel to a mountain belt.Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure.The width and depth of the foreland basin is determined by the flexural rigidity of the underlying ...Back-arc basins are geologic basins, submarine features associated with island arcs and subduction zones.They are found at some convergent plate boundaries, presently concentrated in the western Pacific Ocean.Most of them result from tensional forces caused by oceanic trench rollback (the oceanic trench is wandering in the seafloor direction) and the collapse of the edge of the continent.Forearc, active arc, and back arc are expressed differently on either side of these boundaries (see figure below). The forearc is that part of the arc system between the trench and the magmatic front of the arc and includes uplifted sectors of the forearc situated near the magmatic front, sometimes called the ‘frontal arc’.Forearc is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.The forearc lies between the trench and the volcanic arc. Globally, forearcs have the lowest heatflow from the interior Earth because there is no asthenosphere (convecting mantle) between the forearc lithosphere and the cold subducting plate. [citation needed] The inner trench wall marks the edge of the overriding plate and the outermost forearc.Examples of how to use “forearc” in a sentence from the Cambridge Dictionary Labsforearc (plural forearcs) ( geology ) A region of raised rock debris which forms between the subduction zone and any associated volcano or volcanic chain. Anagrams [ edit ]An older assumption that backstops of accretionary wedges dip back toward the arc, and that accreted material is emplaced below such backstops, is contradicted by observations from many active forearcs that indicate (1) backthrusting is common, (2) forearc basins are nearly ubiquitous associates of accretionary wedges, and (3) forearc basement ...The studies provide new data from the upper mantle to the surface, from the forearc to the active foreland basin, and employ a wide array of techniques and methods in geophysics, petrology, geochronology and thermochronology, sedimentology, structural geology, geomorphology, paleoaltimetry, and geodynamic modeling.

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What is FOREARC? What does FOREARC mean? FOREARC meaning - FOREARC pronunciation - FOREARC definition - FOREARC explanation - How to pronounce FOREARC? Source: article, adapted under ...A forearc or forarc, also called arc-trench gap, [1] is a depression in the sea floor located between a subduction zone and an associated volcanic arc. Typically, it is filled with sediments from the adjacent landmass and the island arc in addition to trapped oceanic crustal material.Wikipedia's Forearc as translated by GramTrans. La ĉi-suba teksto estas aŭtomata traduko de la artikolo Forearc article en la angla Vikipedio, farita per la sistemo GramTrans on 2016-01-31 17:22:20. Eventualaj ŝanĝoj en la angla originalo estos kaptitaj per regulaj retradukoj.The Hellenic arc or Aegean arc is an arcuate tectonic feature of the eastern Mediterranean Sea related to the subduction of the African Plate beneath the Aegean Sea Plate.It consists of an oceanic trench, the Hellenic Trench, on its outer side; two arcs—a non-volcanic outer arc and an inner volcanic arc, the South Aegean Volcanic Arc; and a marginal sea on its inner side.Forearc Basin. Forearc basin forms between the volcanic arc and the trench. Volcanic arc and accretionary prism borders the edge of forearc basin. Dimension of forearc basin depends on the arc-trench gap. Continental margin or oceanic crust may form the base of forearc basin. Concerning its capacity to accumulate sediments, rate of subsidence ...Nappe formations of the Oceanic Formation, from a Miocene forearc basin filled with calcareous pelagic sediments and volcanic ash is thrusted on top of the two older units. Mud, rich in organic molecules intrudes all of these units with diapirs—rising tendrils of mud with behavior similar to salt domes.The Chilean Coastal Range (Spanish: Cordillera de la Costa) is a mountain range that runs from north to south along the Pacific coast of South America parallel to the Andean Mountains, extending from Morro de Arica in the north to Taitao Peninsula, where it ends at the Chile Triple Junction, in the south.The range has a strong influence on the climate of Chile since it produces a rain shadow ...Ranquil Formation (Spanish: Formación Ranquil) is a Miocene and Pliocene sedimentary formation located in Arauco Province in south–central Chile, including outcrops in Mocha Island.The formation has its greatest thicknesses in the south-west, where its sediments were largely deposited in marine conditions.Due to it being less buoyant, the seamount would be less likely to lift up the forearc, which would also cause it to be weakly coupled to the overriding plate as well. This means, the probability this seamount will cause major earthquakes or effect the overall morphology of the forearc would be significantly lessened.Ejemplos de uso de “forearc” en una frase de los Cambridge Dictionary Labs

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