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- W2190804871 abstract "In this study we use crustal-scale Ocean Bottom Seismic models to infer the presence of two types of lower crustal bodies at North Atlantic passive margins; Type I, primarily interpreted as Early Eocene magmatic intrusions, and Type II, interpreted as Caledonian eclogites. We discuss how these eclogites might be related to the main Caledonian Suture Zone and other tectonic features in a conjugate North Atlantic setting. Based on the first-order approximation that P-wave velocities can be related to rock strength, the narrower continental margin at the southern (Møre) transect may be explained by stronger lower crust there, compared with the northern (Vøring) transect. This difference in strength, possibly resulting in a steeper dip in the subducting Baltica Plate south of the proto-Jan Mayen Lineament, may explain the asymmetry in extensional style observed across this lineament. Our interpretation locates the main suture off mid-Norway close to the Møre Trøndelag Fault Zone on the Møre Margin, along the western boundary of the Trøndelag Platform on the Vøring Margin, and further northwards beneath the Lofoten Ridge. The Lower Crustal Body Type I is about 60% thicker on the Greenland side, for both transects, and its thickness along the northern transect is more than twice that of the southern transect. These differences are consistent with sub-lithospheric interaction between the Icelandic hotspot and the continental rift/oceanic accretion system around the time of continental break-up." @default.
- W2190804871 created "2016-06-24" @default.
- W2190804871 creator A5004095776 @default.
- W2190804871 creator A5028100934 @default.
- W2190804871 creator A5051889606 @default.
- W2190804871 creator A5088831781 @default.
- W2190804871 date "2016-02-01" @default.
- W2190804871 modified "2023-10-16" @default.
- W2190804871 title "Lower crustal high-velocity bodies along North Atlantic passive margins, and their link to Caledonian suture zone eclogites and Early Cenozoic magmatism" @default.
- W2190804871 cites W1548890681 @default.
- W2190804871 cites W1553799086 @default.
- W2190804871 cites W1923323481 @default.
- W2190804871 cites W1942113640 @default.
- W2190804871 cites W1964322474 @default.
- W2190804871 cites W1965078451 @default.
- W2190804871 cites W1966841620 @default.
- W2190804871 cites W1966912410 @default.
- W2190804871 cites W1969030365 @default.
- W2190804871 cites W1969242280 @default.
- W2190804871 cites W1972167093 @default.
- W2190804871 cites W1972380754 @default.
- W2190804871 cites W1973891027 @default.
- W2190804871 cites W1977230258 @default.
- W2190804871 cites W1983086091 @default.
- W2190804871 cites W1985757886 @default.
- W2190804871 cites W1987793062 @default.
- W2190804871 cites W1988853556 @default.
- W2190804871 cites W1989072731 @default.
- W2190804871 cites W1990479664 @default.
- W2190804871 cites W1990919062 @default.
- W2190804871 cites W1992060729 @default.
- W2190804871 cites W1992616066 @default.
- W2190804871 cites W1993511896 @default.
- W2190804871 cites W1994323983 @default.
- W2190804871 cites W1994855356 @default.
- W2190804871 cites W1996052457 @default.
- W2190804871 cites W1996514150 @default.
- W2190804871 cites W1997604005 @default.
- W2190804871 cites W2001820253 @default.
- W2190804871 cites W2007206429 @default.
- W2190804871 cites W2009988327 @default.
- W2190804871 cites W2018158894 @default.
- W2190804871 cites W2018314772 @default.
- W2190804871 cites W2018763910 @default.
- W2190804871 cites W2022648729 @default.
- W2190804871 cites W2024005545 @default.
- W2190804871 cites W2024015166 @default.
- W2190804871 cites W2024108081 @default.
- W2190804871 cites W2025599463 @default.
- W2190804871 cites W2025841258 @default.
- W2190804871 cites W2027123291 @default.
- W2190804871 cites W2032236764 @default.
- W2190804871 cites W2032540454 @default.
- W2190804871 cites W2032693613 @default.
- W2190804871 cites W2034251658 @default.
- W2190804871 cites W2034753142 @default.
- W2190804871 cites W2039117036 @default.
- W2190804871 cites W2041668854 @default.
- W2190804871 cites W2041870740 @default.
- W2190804871 cites W2045752704 @default.
- W2190804871 cites W2046640225 @default.
- W2190804871 cites W2046973150 @default.
- W2190804871 cites W2047206863 @default.
- W2190804871 cites W2048179894 @default.
- W2190804871 cites W2050202464 @default.
- W2190804871 cites W2050645730 @default.
- W2190804871 cites W2054561274 @default.
- W2190804871 cites W2056766036 @default.
- W2190804871 cites W2057408414 @default.
- W2190804871 cites W2059777175 @default.
- W2190804871 cites W2060657802 @default.
- W2190804871 cites W2060977915 @default.
- W2190804871 cites W2063328224 @default.
- W2190804871 cites W2064892917 @default.
- W2190804871 cites W2065947578 @default.
- W2190804871 cites W2067349192 @default.
- W2190804871 cites W2067975355 @default.
- W2190804871 cites W2071514600 @default.
- W2190804871 cites W2073485883 @default.
- W2190804871 cites W2074315931 @default.
- W2190804871 cites W2074469711 @default.
- W2190804871 cites W2078646061 @default.
- W2190804871 cites W2078943943 @default.
- W2190804871 cites W2084881015 @default.
- W2190804871 cites W2086373513 @default.
- W2190804871 cites W2094746059 @default.
- W2190804871 cites W2103108238 @default.
- W2190804871 cites W2103523218 @default.
- W2190804871 cites W2107540055 @default.
- W2190804871 cites W2118970168 @default.
- W2190804871 cites W2119297767 @default.
- W2190804871 cites W2122900859 @default.
- W2190804871 cites W2123915079 @default.
- W2190804871 cites W2131839205 @default.
- W2190804871 cites W2132035356 @default.
- W2190804871 cites W2140045893 @default.
- W2190804871 cites W2143641098 @default.
- W2190804871 cites W2149457841 @default.