Matches in SemOpenAlex for { <https://semopenalex.org/work/W2956168316> ?p ?o ?g. }
- W2956168316 endingPage "795" @default.
- W2956168316 startingPage "776" @default.
- W2956168316 abstract "SUMMARY The southcentral Hikurangi subduction margin (North Island, New Zealand) has a wide, low-taper accretionary wedge that is frontally accreting a >3-km-thick layer of sediments, with deformation currently focused near the toe of the wedge. We use a geological model based on a depth-converted seismic section, together with physically realistic parameters for fluid pressure, and sediment and décollement friction based on laboratory experiments, to investigate the present-day force balance in the wedge. Numerical models are used to establish the range of physical parameters compatible with the present-day wedge geometry and mechanics. Our analysis shows that the accretionary wedge stability and taper angle require either high to moderate fluid pressure on the plate interface, and/or weak frictional strength along the décollement. The décollement beneath the outer wedge requires a relatively weaker effective strength than beneath the inner (consolidated) wedge. Increasing density and cohesion with depth make it easier to attain a stable taper within the inner wedge, while anything that weakens the wedge—such as high fluid pressures and weak faults—make it harder. Our results allow a near-hydrostatic wedge fluid pressure, sublithostatic fluid overpressure at the subduction interface, and friction coefficients compatible with measurements from laboratory experiments on weak clay minerals." @default.
- W2956168316 created "2019-07-23" @default.
- W2956168316 creator A5042335151 @default.
- W2956168316 creator A5059446036 @default.
- W2956168316 creator A5064727810 @default.
- W2956168316 creator A5071169545 @default.
- W2956168316 creator A5072954849 @default.
- W2956168316 creator A5088745083 @default.
- W2956168316 date "2019-07-16" @default.
- W2956168316 modified "2023-10-16" @default.
- W2956168316 title "The contemporary force balance in a wide accretionary wedge: numerical models of the southcentral Hikurangi margin of New Zealand" @default.
- W2956168316 cites W1494639822 @default.
- W2956168316 cites W1504500543 @default.
- W2956168316 cites W1510841103 @default.
- W2956168316 cites W1518875880 @default.
- W2956168316 cites W1585318996 @default.
- W2956168316 cites W1776538945 @default.
- W2956168316 cites W1902216953 @default.
- W2956168316 cites W1931506078 @default.
- W2956168316 cites W1945447172 @default.
- W2956168316 cites W1968121614 @default.
- W2956168316 cites W1973618300 @default.
- W2956168316 cites W1975861287 @default.
- W2956168316 cites W1977596365 @default.
- W2956168316 cites W1992718586 @default.
- W2956168316 cites W1995840908 @default.
- W2956168316 cites W1996435354 @default.
- W2956168316 cites W1997950772 @default.
- W2956168316 cites W1999437756 @default.
- W2956168316 cites W2003050391 @default.
- W2956168316 cites W2006115899 @default.
- W2956168316 cites W2009333215 @default.
- W2956168316 cites W2009454183 @default.
- W2956168316 cites W2010985259 @default.
- W2956168316 cites W2016641515 @default.
- W2956168316 cites W2016779250 @default.
- W2956168316 cites W2018896712 @default.
- W2956168316 cites W2019199746 @default.
- W2956168316 cites W2022945770 @default.
- W2956168316 cites W2023665440 @default.
- W2956168316 cites W2025347762 @default.
- W2956168316 cites W2026254189 @default.
- W2956168316 cites W2027253376 @default.
- W2956168316 cites W2027517205 @default.
- W2956168316 cites W2032645520 @default.
- W2956168316 cites W2037465830 @default.
- W2956168316 cites W2047713972 @default.
- W2956168316 cites W2049341401 @default.
- W2956168316 cites W2051340808 @default.
- W2956168316 cites W2052488926 @default.
- W2956168316 cites W2054649362 @default.
- W2956168316 cites W2057319664 @default.
- W2956168316 cites W2060782632 @default.
- W2956168316 cites W2062124496 @default.
- W2956168316 cites W2062785665 @default.
- W2956168316 cites W2063290645 @default.
- W2956168316 cites W2066403878 @default.
- W2956168316 cites W2066853922 @default.
- W2956168316 cites W2080124836 @default.
- W2956168316 cites W2081856232 @default.
- W2956168316 cites W2082469483 @default.
- W2956168316 cites W2088025384 @default.
- W2956168316 cites W2092753394 @default.
- W2956168316 cites W2093390031 @default.
- W2956168316 cites W2095036489 @default.
- W2956168316 cites W2099735302 @default.
- W2956168316 cites W2100824634 @default.
- W2956168316 cites W2105425673 @default.
- W2956168316 cites W2105521914 @default.
- W2956168316 cites W2105791426 @default.
- W2956168316 cites W2110585121 @default.
- W2956168316 cites W2110898916 @default.
- W2956168316 cites W2118781039 @default.
- W2956168316 cites W2124153265 @default.
- W2956168316 cites W2124198179 @default.
- W2956168316 cites W2130833734 @default.
- W2956168316 cites W2133216200 @default.
- W2956168316 cites W2134946466 @default.
- W2956168316 cites W2135257207 @default.
- W2956168316 cites W2135996487 @default.
- W2956168316 cites W2136646307 @default.
- W2956168316 cites W2144609418 @default.
- W2956168316 cites W2147258325 @default.
- W2956168316 cites W2148220198 @default.
- W2956168316 cites W2148232034 @default.
- W2956168316 cites W2149143200 @default.
- W2956168316 cites W2151872226 @default.
- W2956168316 cites W2151934553 @default.
- W2956168316 cites W2153326760 @default.
- W2956168316 cites W2155658064 @default.
- W2956168316 cites W2158666730 @default.
- W2956168316 cites W2162702470 @default.
- W2956168316 cites W2168144057 @default.
- W2956168316 cites W2170255934 @default.
- W2956168316 cites W2172293152 @default.
- W2956168316 cites W2185308876 @default.
- W2956168316 cites W2297963167 @default.
- W2956168316 cites W2317985128 @default.