Matches in SemOpenAlex for { <https://semopenalex.org/work/W4386860358> ?p ?o ?g. }
- W4386860358 endingPage "405" @default.
- W4386860358 startingPage "390" @default.
- W4386860358 abstract "The Eastern European lithosphere is a natural laboratory to study continental formation and evolution through time, comprising Archean continental remnants, Proterozoic rifts and belts, and younger accreted terranes. We investigate the seismic structure of the East European Craton (EEC) crust and uppermost mantle, and the transition from Precambrian to Phanerozoic Europe across the Trans European Suture Zone (TESZ) using probabilistic transdimensional ambient noise tomography. We cross-correlate noise recorded at broadband seismic stations from Eastern, Northern, and Central Europe, remove earthquake signals using continuous wavelet transform, and extract Rayleigh wave phase velocity dispersion curves. We invert these for the highest resolution shear wave velocity model of the Eastern European lithosphere to date, using Markov chain Monte Carlo Bayesian inversion. Our shear wave velocity model exhibits spatial correlation with major tectonic units and bears similarities with active seismic survey profiles in terms of seismic velocity patterns and main discontinuities. The crust thickens across the TESZ boundary and the mantle is seismically faster than beneath younger terranes, consistent with a less dense Precambrian lithosphere in the EEC. The crust and lithosphere beneath the Pannonian region is hyper-extended but the adjacent Transylvanian basin crust shows significant heterogeneity. The Precambrian building blocks of the EEC exhibit contrasting seismic fabrics. The Baltic orogens of Fennoscandia are underlain by uniform crust with a flat Moho, while Sarmatia shows alternating high and low velocity layers and a regional south-dipping crustal boundary from beneath the Ukrainian Shield towards the Crimean Peninsula. The last observation supports a geodynamic style driven by horizontal rather than vertical tectonics, with fundamental implications for the formation and evolution of early continents." @default.
- W4386860358 created "2023-09-20" @default.
- W4386860358 creator A5002414936 @default.
- W4386860358 creator A5016363945 @default.
- W4386860358 creator A5039561144 @default.
- W4386860358 creator A5040690507 @default.
- W4386860358 creator A5043766129 @default.
- W4386860358 creator A5066761626 @default.
- W4386860358 date "2024-01-01" @default.
- W4386860358 modified "2023-09-30" @default.
- W4386860358 title "Seismic structure of the Eastern European crust and upper mantle from probabilistic ambient noise tomography" @default.
- W4386860358 cites W1262883574 @default.
- W4386860358 cites W1492924402 @default.
- W4386860358 cites W1582044806 @default.
- W4386860358 cites W1599507010 @default.
- W4386860358 cites W1840277268 @default.
- W4386860358 cites W1845351382 @default.
- W4386860358 cites W1965172693 @default.
- W4386860358 cites W1965694483 @default.
- W4386860358 cites W1970845006 @default.
- W4386860358 cites W1973012528 @default.
- W4386860358 cites W1974728100 @default.
- W4386860358 cites W1978300007 @default.
- W4386860358 cites W1983912640 @default.
- W4386860358 cites W1988046698 @default.
- W4386860358 cites W1988914543 @default.
- W4386860358 cites W1995290085 @default.
- W4386860358 cites W1995444953 @default.
- W4386860358 cites W1997243017 @default.
- W4386860358 cites W1998447897 @default.
- W4386860358 cites W1998515186 @default.
- W4386860358 cites W1998595915 @default.
- W4386860358 cites W2001939799 @default.
- W4386860358 cites W2007056155 @default.
- W4386860358 cites W2007704528 @default.
- W4386860358 cites W2008126095 @default.
- W4386860358 cites W2009286275 @default.
- W4386860358 cites W2009353958 @default.
- W4386860358 cites W2012564583 @default.
- W4386860358 cites W2016408382 @default.
- W4386860358 cites W2017846713 @default.
- W4386860358 cites W2018314772 @default.
- W4386860358 cites W2023500412 @default.
- W4386860358 cites W2025669066 @default.
- W4386860358 cites W2026361339 @default.
- W4386860358 cites W2027461823 @default.
- W4386860358 cites W2030866924 @default.
- W4386860358 cites W2031395330 @default.
- W4386860358 cites W2031458587 @default.
- W4386860358 cites W2035869936 @default.
- W4386860358 cites W2039669657 @default.
- W4386860358 cites W2039762361 @default.
- W4386860358 cites W2040123418 @default.
- W4386860358 cites W2040829729 @default.
- W4386860358 cites W2043695697 @default.
- W4386860358 cites W2043804156 @default.
- W4386860358 cites W2045040002 @default.
- W4386860358 cites W2046650100 @default.
- W4386860358 cites W2047988432 @default.
- W4386860358 cites W2048893847 @default.
- W4386860358 cites W2052504895 @default.
- W4386860358 cites W2053761888 @default.
- W4386860358 cites W2056952143 @default.
- W4386860358 cites W2060335907 @default.
- W4386860358 cites W2067408083 @default.
- W4386860358 cites W2068564701 @default.
- W4386860358 cites W2072323721 @default.
- W4386860358 cites W2079102241 @default.
- W4386860358 cites W2084356588 @default.
- W4386860358 cites W2091202638 @default.
- W4386860358 cites W2094997444 @default.
- W4386860358 cites W2095965656 @default.
- W4386860358 cites W2097897435 @default.
- W4386860358 cites W2101148475 @default.
- W4386860358 cites W2104133227 @default.
- W4386860358 cites W2108649875 @default.
- W4386860358 cites W2110201400 @default.
- W4386860358 cites W2112962547 @default.
- W4386860358 cites W2113559499 @default.
- W4386860358 cites W2113778426 @default.
- W4386860358 cites W2115497827 @default.
- W4386860358 cites W2123205872 @default.
- W4386860358 cites W2130458857 @default.
- W4386860358 cites W2132119502 @default.
- W4386860358 cites W2132300453 @default.
- W4386860358 cites W2136463069 @default.
- W4386860358 cites W2139713088 @default.
- W4386860358 cites W2146924389 @default.
- W4386860358 cites W2155333935 @default.
- W4386860358 cites W2155417312 @default.
- W4386860358 cites W2156688953 @default.
- W4386860358 cites W2160717452 @default.
- W4386860358 cites W2161726009 @default.
- W4386860358 cites W2169396008 @default.
- W4386860358 cites W2171163720 @default.
- W4386860358 cites W2193771126 @default.
- W4386860358 cites W2280285828 @default.
- W4386860358 cites W2286174841 @default.