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• W2050292131 endingPage "12106" @default.
• W2050292131 startingPage "12081" @default.
• W2050292131 abstract "Shear wave velocity, especially when used with Compressional wave velocity, is an important constraint on estimates of the composition and physical state of the continental lithosphere. We present shear velocity (ν s ) models derived from high‐quality S wave data along three profiles in Southwest Germany, which combine with existing P wave velocity (ν p ) models to give Poisson's ratio (σ) in the crust and uppermost mantle. We then construct a laterally varying petrological model of the crust by comparing our ν p and ν s models with published laboratory‐measured rock velocities. In general, Poisson's ratio is 0.25 in the uppermost crust, 0.22–0.23 in the mid‐crust (but reaching a low of 0.15 in the Black Forest low‐ν p zone), and varies laterally from 0.24 to 0.30 in the lower crust; the average Poisson's ratio of the whole crust is everywhere about 0.25. The laminated signature of the lower crust prominent on reflection and P wave refraction data is absent on the S wave refraction data, implying a strong high/low alternation of Poisson's ratio in the lower crust. This suggests that the lower‐crustal laminae represent mafic/silicic compositional layering (for example, basic sills in an originally more quartz‐rich lower crust) rather than alternating zones of high and low pore pressure. There is no evidence for a shear wave low‐velocity zone (LVZ) in the Black Forest mid‐crust, despite the presence of a strong P wave LVZ; this suggests high quartz content and the presence of pore fluids at low (not high) pore pressure. A clear P ‐to‐ S converted Moho reflection ( P m S ) is visible on several shots, indicating that the Moho is, at least locally, a first‐order discontinuity. No shear wave refractions from the upper mantle are present, even where strong P wave refractions are observed, possibly indicating an increase of Poisson's ratio with depth in the upper mantle. The petrological modeling indicates that the upper and middle crust are probably of granitic composition, that the mid‐crustal low‐ν p zones have high quartz content, and that the lower crust probably consists of granulites of laterally varying bulk composition, from granodioritic to gabbroic. The lower crust is more mafic in areas of high reflection density on seismic reflection profiles, suggesting that the laminations are caused by mafic intrusions into the lower crust, either prior to the Variscan orogeny or during (Tertiary?) volcanic activity." @default.
• W2050292131 created "2016-06-24" @default.
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• W2050292131 date "1988-10-10" @default.
• W2050292131 modified "2023-10-13" @default.
• W2050292131 title "An interpretation of wide‐angle compressional and shear wave data in southwest Germany: Poisson's ratio and petrological implications" @default.
• W2050292131 cites W1488731268 @default.
• W2050292131 cites W1495262655 @default.
• W2050292131 cites W1498318358 @default.
• W2050292131 cites W1521494680 @default.
• W2050292131 cites W1535014139 @default.
• W2050292131 cites W1550440361 @default.
• W2050292131 cites W1562913330 @default.
• W2050292131 cites W1669523593 @default.
• W2050292131 cites W1964378450 @default.
• W2050292131 cites W1972720261 @default.
• W2050292131 cites W1984168258 @default.
• W2050292131 cites W1985756592 @default.
• W2050292131 cites W1989505097 @default.
• W2050292131 cites W1993959695 @default.
• W2050292131 cites W1999288300 @default.
• W2050292131 cites W1999627522 @default.
• W2050292131 cites W2001823899 @default.
• W2050292131 cites W2003584308 @default.
• W2050292131 cites W2005789596 @default.
• W2050292131 cites W2007097118 @default.
• W2050292131 cites W2009280412 @default.
• W2050292131 cites W2009799761 @default.
• W2050292131 cites W2011644456 @default.
• W2050292131 cites W2014878983 @default.
• W2050292131 cites W2017664549 @default.
• W2050292131 cites W2018528944 @default.
• W2050292131 cites W2019176073 @default.
• W2050292131 cites W2025802367 @default.
• W2050292131 cites W2030933415 @default.
• W2050292131 cites W2033054510 @default.
• W2050292131 cites W2034750078 @default.
• W2050292131 cites W2038120870 @default.
• W2050292131 cites W2038127544 @default.
• W2050292131 cites W2041033683 @default.
• W2050292131 cites W2046528803 @default.
• W2050292131 cites W2048127257 @default.
• W2050292131 cites W2050730624 @default.
• W2050292131 cites W2051357081 @default.
• W2050292131 cites W2052535287 @default.
• W2050292131 cites W2052917016 @default.
• W2050292131 cites W2060293298 @default.
• W2050292131 cites W2066960124 @default.
• W2050292131 cites W2069477573 @default.
• W2050292131 cites W2071596657 @default.
• W2050292131 cites W2072929359 @default.
• W2050292131 cites W2075378929 @default.
• W2050292131 cites W2076670951 @default.
• W2050292131 cites W2087295055 @default.
• W2050292131 cites W2094997444 @default.
• W2050292131 cites W2097334536 @default.
• W2050292131 cites W2097510110 @default.
• W2050292131 cites W2101926655 @default.
• W2050292131 cites W2107334329 @default.
• W2050292131 cites W2108018879 @default.
• W2050292131 cites W2111068345 @default.
• W2050292131 cites W2116536971 @default.
• W2050292131 cites W2119795805 @default.
• W2050292131 cites W2135544805 @default.
• W2050292131 cites W2139444382 @default.
• W2050292131 cites W2142980354 @default.
• W2050292131 cites W2143744241 @default.
• W2050292131 cites W2153615532 @default.
• W2050292131 cites W2156786968 @default.
• W2050292131 cites W2163725799 @default.
• W2050292131 cites W2165258323 @default.
• W2050292131 cites W2166026905 @default.
• W2050292131 cites W2167047272 @default.
• W2050292131 cites W2169032677 @default.
• W2050292131 cites W2169634156 @default.
• W2050292131 cites W2169997237 @default.
• W2050292131 cites W2188969689 @default.
• W2050292131 cites W2229805401 @default.
• W2050292131 cites W2321538211 @default.
• W2050292131 cites W4234926460 @default.
• W2050292131 cites W4255496497 @default.
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• W2050292131 doi "https://doi.org/10.1029/jb093ib10p12081" @default.
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