Anagram & Information om | Engelska ordet FOREARC

Exempel på hur man kan använda FOREARC i en mening

• Due to collisional stresses as one tectonic plate subducts under another, forearc regions are sources for powerful earthquakes.
• This chain, which resurfaces in Nusa Tenggara in the mountainous islands of Sumba and Timor, is the forearc of the South Sumatra Basin along the Sunda Trench subduction zone.
• The forearc of the Marianas subduction zone hosts large serpentinite mud volcanoes, which erupt serpentinite mud that rises through faults from the underlying serpentinized forearc mantle.
• Volcanogenic massive sulfide deposits are forming today on the seafloor around undersea volcanoes along many mid ocean ridges, and within back-arc basins and forearc rifts.
• The schist may represent subducted Valdez Group that was exhumed in the forearc region from beneath the Peninsular terrane.
• A forearc environment is ideal for boninite genesis, but other tectonic environments, such as backarcs, might be able to form boninite.
• The range has no single structural or lithological origin but is the result of the alignment of horst, forearc highs and upthrusted blocks along Chile's coast.
• The shales (and slates) of the Martinsburg were deposited in a large forearc basin resulting in a flysch deposit.
• According to McCaffrey, this is fast enough to have produced geologically significant effects, such as unroofing of high-grade metamorphic rocks, and provides one explanation for why the forearc in southern IBM is tectonically more active than that in northern IBM.
• Detached ophiolitic series and thick melanges are overlain by forearc deposits; subduction-driven east–west shortening of the Snellius Plateau caused the thrust melanges to reactivate and deform the forearc series.
• It consists of marine forearc basin sediments, typically turbiditic and bioturbated mudstones and sandstones with subordinate conglomerate primarily deposited on the continental shelf and slope of the ancient Yezo subduction margin.
• The Murihiku Terrane is considered to be an accretionary wedge of mainly volcanogenic forearc sediments.
• The Murihiku Terrane is considered to be an accretionary wedge of mainly volcanogenic forearc sediments.
• During subduction the western end of the forearc region flexured downward forming a giant monocline.
• Perhaps the bottom of the trench did not connect with (was decoupled from) the subducting plate at all but was a "pull apart" fault basin in the forearc (the raised chain of highlands and islands), or perhaps it was part of a wrinkle in the foredeep produced by compressional motion of the Aegean Plate against the "backstop" of the Mediterranean Ridge.
• The subsiding segment of the Philippine Plate is the so-called ‘Shikoku basin’, which defines a former forearc basin that was subsequently filled with sediments from submarine fan systems in the area, although most of the accreted sediments consist of coarse terrestrial clastics.
• As the subducting slab shallowed, crustal garnet-containing lherzolite and granulite-eclogite—contributed both from the crustal basis and forearc rocks that were dragged down by the subducting slab—became an increasingly important component of erupted magmas.
• Other phenomena which coincide with the Pica gap are the absence of tectonic horsts west of the Andes, an area where a zone of high electrical conductivity in the deep crust beneath the forearc does not extend to the actual volcanic arc (and thus may reflect the absence of molten magma), the lack of a low seismic velocity zone in the crust, a symmetry plane of the Andes, the Salar de Uyuni basin behind the arc and the location of the actual bend in the Andes that is usually placed at the Arica Bend.
• Stern has led or participated in many marine geoscientific expeditions in the Mariana convergent margin, exploring most of the submarine arc volcanoes by dredging and ROV studies; deeper regions in the backarc basin and forearc have been studied by dredging and diving with manned submersible.
• The Thong Pha Phum Group conformably overlies the Thung Song Group in the west with a thick sequence of non-fossil bearing clastic marine sedimentary rocks that likely deposited in a forearc basin.

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