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• W2038586835 abstract "[1] The Hellenic Arc of Greece is the most seismically active part of Europe, but little is know about its mechanics. We modeled deformation along the arc using a finite element model. The model was intended to capture large-scale 3-D structure of Nubian plate subduction beneath the Aegean block and its deformational consequences. The shape of the interface was developed using mapped traces at the surface and earthquake hypocenters at depth. Model block motions were constrained by recent compilations of GPS velocity vectors. We simulated a 10 ka period of convergence between Nubia and the Aegean and calculated the strain field in the overriding plate as well as the spatial distribution and orientation of differential stress (∣σ1 − σ3∣). From these calculations we derived testable quantities such as the expected seismic moment rate on the interplate contact, uplift pattern, and distribution of strain modes. Our relatively simple model broadly reproduced observed uplift patterns, earthquake activity, and loci of extension and contraction. The model showed a localization of uplift near the island of Crete, where the fastest Aegean uplift rates are well documented. Comparison of calculated expected seismic moment and observed earthquake catalogs implies a nearly fully coupled interplate contact. On the basis of our modeling results, we suggest that south Aegean deformation is driven primarily by the fast moving (∼33 mm a−1) Aegean upper plate overriding a nearly stalled (∼5 mm a−1) Nubian lower plate. This tectonic setting thus more closely resembles a continental thrust than it does a typical oceanic subduction zone." @default.
• W2038586835 created "2016-06-24" @default.
• W2038586835 creator A5008557220 @default.
• W2038586835 creator A5084232501 @default.
• W2038586835 date "2009-06-20" @default.
• W2038586835 modified "2023-10-03" @default.
• W2038586835 title "Three-dimensional model of Hellenic Arc deformation and origin of the Cretan uplift" @default.
• W2038586835 cites W146294249 @default.
• W2038586835 cites W1484450406 @default.
• W2038586835 cites W1575777612 @default.
• W2038586835 cites W1589900634 @default.
• W2038586835 cites W1590043396 @default.
• W2038586835 cites W1616181869 @default.
• W2038586835 cites W1889512547 @default.
• W2038586835 cites W1924018542 @default.
• W2038586835 cites W1971708483 @default.
• W2038586835 cites W1977216678 @default.
• W2038586835 cites W1979536782 @default.
• W2038586835 cites W1979870348 @default.
• W2038586835 cites W1981165981 @default.
• W2038586835 cites W1982460134 @default.
• W2038586835 cites W1983926551 @default.
• W2038586835 cites W1984039516 @default.
• W2038586835 cites W1986558800 @default.
• W2038586835 cites W1986681588 @default.
• W2038586835 cites W1986926008 @default.
• W2038586835 cites W1987031963 @default.
• W2038586835 cites W1996043771 @default.
• W2038586835 cites W1999007384 @default.
• W2038586835 cites W1999685964 @default.
• W2038586835 cites W2001820253 @default.
• W2038586835 cites W2002485032 @default.
• W2038586835 cites W2004153174 @default.
• W2038586835 cites W2006495189 @default.
• W2038586835 cites W2007814542 @default.
• W2038586835 cites W2014680155 @default.
• W2038586835 cites W2014907217 @default.
• W2038586835 cites W2015144933 @default.
• W2038586835 cites W2015739117 @default.
• W2038586835 cites W2015934892 @default.
• W2038586835 cites W2025841258 @default.
• W2038586835 cites W2027518639 @default.
• W2038586835 cites W2029022233 @default.
• W2038586835 cites W2034066217 @default.
• W2038586835 cites W2039641351 @default.
• W2038586835 cites W2040800160 @default.
• W2038586835 cites W2043474718 @default.
• W2038586835 cites W2045147022 @default.
• W2038586835 cites W2045553384 @default.
• W2038586835 cites W2046285342 @default.
• W2038586835 cites W2052897582 @default.
• W2038586835 cites W2054060475 @default.
• W2038586835 cites W2054591717 @default.
• W2038586835 cites W2054793434 @default.
• W2038586835 cites W2056754262 @default.
• W2038586835 cites W2056967965 @default.
• W2038586835 cites W2057526825 @default.
• W2038586835 cites W2064893459 @default.
• W2038586835 cites W2065794688 @default.
• W2038586835 cites W2069921444 @default.
• W2038586835 cites W2071786173 @default.
• W2038586835 cites W2076464192 @default.
• W2038586835 cites W2077473835 @default.
• W2038586835 cites W2078374721 @default.
• W2038586835 cites W2078697168 @default.
• W2038586835 cites W2079540099 @default.
• W2038586835 cites W2082482423 @default.
• W2038586835 cites W2087942386 @default.
• W2038586835 cites W2088463293 @default.
• W2038586835 cites W2091137804 @default.
• W2038586835 cites W2092068439 @default.
• W2038586835 cites W2093947124 @default.
• W2038586835 cites W2096775326 @default.
• W2038586835 cites W2097509823 @default.
• W2038586835 cites W2097570511 @default.
• W2038586835 cites W2101777694 @default.
• W2038586835 cites W2108521062 @default.
• W2038586835 cites W2111350198 @default.
• W2038586835 cites W2115395904 @default.
• W2038586835 cites W2117153052 @default.
• W2038586835 cites W2118184448 @default.
• W2038586835 cites W2120122408 @default.
• W2038586835 cites W2124347931 @default.
• W2038586835 cites W2129992518 @default.
• W2038586835 cites W2130014760 @default.
• W2038586835 cites W2133274607 @default.
• W2038586835 cites W2134461822 @default.
• W2038586835 cites W2136633733 @default.
• W2038586835 cites W2138137515 @default.
• W2038586835 cites W2145343103 @default.
• W2038586835 cites W2145786970 @default.
• W2038586835 cites W2152005341 @default.
• W2038586835 cites W2155472085 @default.
• W2038586835 cites W2156301488 @default.
• W2038586835 cites W2156701839 @default.
• W2038586835 cites W2157184090 @default.
• W2038586835 cites W2158650366 @default.
• W2038586835 cites W2162077393 @default.
• W2038586835 cites W2165457450 @default.
• W2038586835 cites W2166074915 @default.

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