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  2. Forearc - Wikipedia

    en.wikipedia.org/wiki/Forearc

    A forearc is a region in a subduction zone between an oceanic trench and the associated volcanic arc. Forearc regions are present along convergent margins and eponymously form 'in front of' the volcanic arcs that are characteristic of convergent plate margins.

  3. Accretionary wedge - Wikipedia

    en.wikipedia.org/wiki/Accretionary_wedge

    Material exposed in the forearc ridge may include fragments of oceanic crust or high pressure metamorphic rocks thrust from deeper in the subduction zone. Elevated regions within the ocean basins such as linear island chains, ocean ridges , and small crustal fragments (such as Madagascar or Japan), known as terranes , are transported toward the ...

  4. Tyrrhenian Basin - Wikipedia

    en.wikipedia.org/wiki/Tyrrhenian_Basin

    The Tyrrhenian Basin is a sedimentary basin located in the western Mediterranean Sea under the Tyrrhenian Sea.It covers a 231,000 km 2 area that is bounded by Sardinia to the west, Corsica to the northwest, Sicily to the southeast, and peninsular Italy to the northeast.

  5. Tectonic subsidence - Wikipedia

    en.wikipedia.org/wiki/Tectonic_subsidence

    Tectonic subsidence is the sinking of the Earth's crust on a large scale, relative to crustal-scale features or the geoid. [1] The movement of crustal plates and accommodation spaces produced by faulting [2] brought about subsidence on a large scale in a variety of environments, including passive margins, aulacogens, fore-arc basins, foreland basins, intercontinental basins and pull-apart basins.

  6. Back-arc basin - Wikipedia

    en.wikipedia.org/wiki/Back-arc_basin

    As the subduction zone and its associated trench pull backward, the overriding plate is stretched, thinning the crust and forming a back-arc basin. In some cases, extension is triggered by the entrance of a buoyant feature in the subduction zone, which locally slows down subduction and induces the subducting plate to rotate adjacent to it.

  7. Geology of Sicily - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Sicily

    The collision of Africa and Eurasia is a retreating subduction system, such that the descending Africa is falling away from Eurasia, and Eurasia extends and fills the space as the African plate falls into the mantle, resulting in volcanic activity in Sicily and the formation of Tyrrhenian slab to the north. [4]

  8. 10 Foods That Famous Chefs Refuse To Eat - AOL

    www.aol.com/10-foods-famous-chefs-refuse...

    3. Truffle Oil – Martha Stewart. Truffle oil is your ingredient to make food instantly classy—or, more accurately, expensive. However, its rather pungent flavor isn’t for everyone, and it ...

  9. Cook Inlet Basin - Wikipedia

    en.wikipedia.org/wiki/Cook_Inlet_Basin

    It separates the forearc basin from the subduction complex as well as deformed metamorphic rocks from the subduction complex. [4] The Fault system originated during the pre-miocene period as a result of megathrust subduction and it was subsequently filled with turbidity deposits. Since then, it underwent contractional deformation in the ...