Matches in SemOpenAlex for { <https://semopenalex.org/work/W4283449509> ?p ?o ?g. }
- W4283449509 abstract "Abstract We document an exhumed plate boundary shear zone—a subduction channel—developed at the contact between a fossil Cretaceous‐Eocene accretionary prism (Ligurian Units) and the underlying continent‐derived nappes of the Northern Apennines. The subduction channel, referred to as the Norsi‐Cavo Complex (NCC), is continuously exposed for ∼10 km along strike on the island of Elba. The NCC consists of oceanic sediments and serpentinites, coupled at the base of the prism. In its northernmost exposures the NCC crops out as a serpentinite mélange with blocks of sedimentary rocks. There, evidence of pervasive fluid‐rock interaction is present. We interpret this mélange as the result of material transfer from the upper plate to the subduction channel through tectonic erosion at the base of the prism. The southern part of the NCC preserves a series of tectonic slices of shales and limestones (Palombini shales) coupled with ultramafic rocks through serpentinite shear zones containing lenses of massive serpentinites, mafic rocks, and sediments. Since sedimentary slices preserve the same structures of the overlying Ligurian Units, produced by accretionary prism deformation, we interpret this complex as the result of material transfer from the prism to the subduction channel and its subsequent underplating at the base of the prism. Based on our interpretation, the NCC fossil subduction channel formed during E‐verging deformation over the W‐directed subduction of the Ligurian Ocean during the early development stages of the Apennines. This deformation terminated when the continental margin entered the subduction." @default.
- W4283449509 created "2022-06-26" @default.
- W4283449509 creator A5013060805 @default.
- W4283449509 creator A5039268898 @default.
- W4283449509 creator A5075750264 @default.
- W4283449509 creator A5079690870 @default.
- W4283449509 date "2022-07-01" @default.
- W4283449509 modified "2023-09-27" @default.
- W4283449509 title "Deformation and Material Transfer in a Fossil Subduction Channel: Evidence From the Island of Elba (Italy)" @default.
- W4283449509 cites W1498453939 @default.
- W4283449509 cites W1507568804 @default.
- W4283449509 cites W1508273826 @default.
- W4283449509 cites W1511178032 @default.
- W4283449509 cites W1522253688 @default.
- W4283449509 cites W1573477650 @default.
- W4283449509 cites W1586083556 @default.
- W4283449509 cites W1602043224 @default.
- W4283449509 cites W1847069267 @default.
- W4283449509 cites W1949478573 @default.
- W4283449509 cites W1965668058 @default.
- W4283449509 cites W1969148653 @default.
- W4283449509 cites W1969384727 @default.
- W4283449509 cites W1975681542 @default.
- W4283449509 cites W1976229064 @default.
- W4283449509 cites W1979698101 @default.
- W4283449509 cites W1979699219 @default.
- W4283449509 cites W1982274789 @default.
- W4283449509 cites W1984339773 @default.
- W4283449509 cites W1989509352 @default.
- W4283449509 cites W1989785208 @default.
- W4283449509 cites W1989983280 @default.
- W4283449509 cites W1998605136 @default.
- W4283449509 cites W1998656861 @default.
- W4283449509 cites W2001538236 @default.
- W4283449509 cites W2007734001 @default.
- W4283449509 cites W2008087815 @default.
- W4283449509 cites W2016190794 @default.
- W4283449509 cites W2016383795 @default.
- W4283449509 cites W2017877780 @default.
- W4283449509 cites W2018036983 @default.
- W4283449509 cites W2022586343 @default.
- W4283449509 cites W2025305480 @default.
- W4283449509 cites W2025364748 @default.
- W4283449509 cites W2026889131 @default.
- W4283449509 cites W2027274494 @default.
- W4283449509 cites W2032437327 @default.
- W4283449509 cites W2034890691 @default.
- W4283449509 cites W2039064764 @default.
- W4283449509 cites W2039142208 @default.
- W4283449509 cites W2040679221 @default.
- W4283449509 cites W2041884579 @default.
- W4283449509 cites W2045047354 @default.
- W4283449509 cites W2051566185 @default.
- W4283449509 cites W2052528966 @default.
- W4283449509 cites W2053799125 @default.
- W4283449509 cites W2054747879 @default.
- W4283449509 cites W2056610596 @default.
- W4283449509 cites W2058083832 @default.
- W4283449509 cites W2058219615 @default.
- W4283449509 cites W2061976920 @default.
- W4283449509 cites W2062312169 @default.
- W4283449509 cites W2063240745 @default.
- W4283449509 cites W2063503947 @default.
- W4283449509 cites W2065768478 @default.
- W4283449509 cites W2066073101 @default.
- W4283449509 cites W2067034804 @default.
- W4283449509 cites W2069938474 @default.
- W4283449509 cites W2071979605 @default.
- W4283449509 cites W2073410054 @default.
- W4283449509 cites W2075190033 @default.
- W4283449509 cites W2078458138 @default.
- W4283449509 cites W2082677624 @default.
- W4283449509 cites W2088282694 @default.
- W4283449509 cites W2088547125 @default.
- W4283449509 cites W2094451024 @default.
- W4283449509 cites W2095441492 @default.
- W4283449509 cites W2099395631 @default.
- W4283449509 cites W2100653978 @default.
- W4283449509 cites W2104885355 @default.
- W4283449509 cites W2114398259 @default.
- W4283449509 cites W2124153265 @default.
- W4283449509 cites W2134436270 @default.
- W4283449509 cites W2139047944 @default.
- W4283449509 cites W2146803029 @default.
- W4283449509 cites W2148232034 @default.
- W4283449509 cites W2156556475 @default.
- W4283449509 cites W2158648190 @default.
- W4283449509 cites W2162495735 @default.
- W4283449509 cites W2163475804 @default.
- W4283449509 cites W2164637250 @default.
- W4283449509 cites W2165617031 @default.
- W4283449509 cites W2167517487 @default.
- W4283449509 cites W2170559182 @default.
- W4283449509 cites W2174523380 @default.
- W4283449509 cites W2259645488 @default.
- W4283449509 cites W2312512653 @default.
- W4283449509 cites W2315365708 @default.
- W4283449509 cites W2316369820 @default.
- W4283449509 cites W2318102871 @default.
- W4283449509 cites W2324831244 @default.