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• W1924532770 endingPage "3715" @default.
• W1924532770 startingPage "3697" @default.
• W1924532770 abstract "Abstract In nature, subducting slabs and overriding plate segments bordering subduction zones are generally embedded within larger plates. Such large plates can impose far‐field boundary conditions that influence the style of subduction and overriding plate deformation. Here we present dynamic laboratory models of progressive subduction in three‐dimensional space, in which the far‐field boundary conditions at the trailing edges of the subducting plate (SP) and overriding plate (OP) are varied. Four configurations are presented: Free (both plates free), SP‐Fixed, OP‐Fixed, and SP‐OP‐Fixed. We investigate their impact on the kinematics and dynamics of subduction, particularly focusing on overriding plate deformation. The results indicate that the variation in far‐field boundary conditions has an influence on the slab geometry, subduction partitioning, and trench migration partitioning. Our models also indicate that in natural (narrow) subduction zones, assuming a homogeneous overriding plate, the formation of back‐arc basins (e.g., Tyrrhenian Sea, Aegean Sea, and Scotia Sea) is generally expected to occur at a comparable location (250–700 km from the trench), irrespective of the boundary condition. In addition, our models indicate that the style of fore‐arc deformation (shortening or extension) is influenced by the mobility of the overriding plate through controlling the force normal to the subduction zone interface (trench suction). Our geodynamic model that uses the SP‐OP‐Fixed setup is comparable to the Calabria subduction zone with respect to subduction kinematics, slab geometry, trench curvature, and accretionary configuration. Furthermore, the model can explain back‐arc and fore‐arc extension at the Calabria subduction zone since the latest middle Miocene as a consequence of subduction of the narrow Calabrian slab and the immobility of the subducting African plate and overriding Eurasian plate. This setting induced strong trench suction, driving fore‐arc extension, and forced subduction to be accommodated almost entirely by slab rollback (not trenchward subducting plate motion), while trench retreat was accommodated almost entirely by back‐arc and fore‐arc extension (not trenchward overriding plate motion), comparable to our SP‐OP‐Fixed model." @default.
• W1924532770 created "2016-06-24" @default.
• W1924532770 creator A5018307892 @default.
• W1924532770 creator A5061436467 @default.
• W1924532770 creator A5087725531 @default.
• W1924532770 date "2015-10-01" @default.
• W1924532770 modified "2023-10-03" @default.
• W1924532770 title "Overriding plate deformation and variability of fore‐arc deformation during subduction: Insight from geodynamic models and application to the <scp>C</scp>alabria subduction zone" @default.
• W1924532770 cites W1544332985 @default.
• W1924532770 cites W1559468888 @default.
• W1924532770 cites W1584792153 @default.
• W1924532770 cites W1595757449 @default.
• W1924532770 cites W1597579421 @default.
• W1924532770 cites W1650398216 @default.
• W1924532770 cites W1660805619 @default.
• W1924532770 cites W1666425291 @default.
• W1924532770 cites W1673724599 @default.
• W1924532770 cites W1676343945 @default.
• W1924532770 cites W1714529472 @default.
• W1924532770 cites W1781608132 @default.
• W1924532770 cites W1825982341 @default.
• W1924532770 cites W1858461780 @default.
• W1924532770 cites W1942772184 @default.
• W1924532770 cites W1966667510 @default.
• W1924532770 cites W1968367915 @default.
• W1924532770 cites W1970807111 @default.
• W1924532770 cites W1971937803 @default.
• W1924532770 cites W1971998696 @default.
• W1924532770 cites W1975613234 @default.
• W1924532770 cites W1976136523 @default.
• W1924532770 cites W1977068211 @default.
• W1924532770 cites W1981230204 @default.
• W1924532770 cites W1982075335 @default.
• W1924532770 cites W1983413696 @default.
• W1924532770 cites W1988048799 @default.
• W1924532770 cites W1989328364 @default.
• W1924532770 cites W1990876884 @default.
• W1924532770 cites W1996435354 @default.
• W1924532770 cites W1996650279 @default.
• W1924532770 cites W1998378006 @default.
• W1924532770 cites W1998926074 @default.
• W1924532770 cites W1999083398 @default.
• W1924532770 cites W2003278850 @default.
• W1924532770 cites W2008110802 @default.
• W1924532770 cites W2011006702 @default.
• W1924532770 cites W2011893217 @default.
• W1924532770 cites W2011898370 @default.
• W1924532770 cites W2015503578 @default.
• W1924532770 cites W2017441826 @default.
• W1924532770 cites W2017663395 @default.
• W1924532770 cites W2020668157 @default.
• W1924532770 cites W2021926110 @default.
• W1924532770 cites W2026863429 @default.
• W1924532770 cites W2028255501 @default.
• W1924532770 cites W2030834466 @default.
• W1924532770 cites W2032047436 @default.
• W1924532770 cites W2033884373 @default.
• W1924532770 cites W2034383653 @default.
• W1924532770 cites W2035732572 @default.
• W1924532770 cites W2039641351 @default.
• W1924532770 cites W2043257593 @default.
• W1924532770 cites W2048567254 @default.
• W1924532770 cites W2051704997 @default.
• W1924532770 cites W2058410734 @default.
• W1924532770 cites W2064604200 @default.
• W1924532770 cites W2064773716 @default.
• W1924532770 cites W2064893459 @default.
• W1924532770 cites W2067485740 @default.
• W1924532770 cites W2070229083 @default.
• W1924532770 cites W2070299474 @default.
• W1924532770 cites W2070501546 @default.
• W1924532770 cites W2071786173 @default.
• W1924532770 cites W2071967664 @default.
• W1924532770 cites W2080750169 @default.
• W1924532770 cites W2081696323 @default.
• W1924532770 cites W2086913022 @default.
• W1924532770 cites W2088282694 @default.
• W1924532770 cites W2089210365 @default.
• W1924532770 cites W2092605097 @default.
• W1924532770 cites W2097657870 @default.
• W1924532770 cites W2100340179 @default.
• W1924532770 cites W2100510409 @default.
• W1924532770 cites W2103819079 @default.
• W1924532770 cites W2108736495 @default.
• W1924532770 cites W2109328511 @default.
• W1924532770 cites W2112052791 @default.
• W1924532770 cites W2114218473 @default.
• W1924532770 cites W2116831667 @default.
• W1924532770 cites W2118197212 @default.
• W1924532770 cites W2120707785 @default.
• W1924532770 cites W2125802704 @default.
• W1924532770 cites W2140809387 @default.
• W1924532770 cites W2142331488 @default.
• W1924532770 cites W2149927268 @default.
• W1924532770 cites W2154603570 @default.
• W1924532770 cites W2156954089 @default.
• W1924532770 cites W2163475804 @default.
• W1924532770 cites W2166479008 @default.

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