FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1991325145> ?p ?o ?g. }

• W1991325145 endingPage "115" @default.
• W1991325145 startingPage "108" @default.
• W1991325145 abstract "The structure and evolution of the Trans-European Suture zone (TESZ), contact between Precambrian Europe to the northeast and Phanerozoic terranes to the southwest is one of the main tectonic questions in Europe. The knowledge of the crustal structure, lithosphere–asthenosphere boundary and mantle transition zone between two seismic discontinuities at depths “410” and “660” km, is one of the most important issues to understand the Earth's dynamics. To create a mantle model of the TESZ and surroundings we used different seismic data collected along the 950 km long POLONAISE'97 profile P4. Previous results of 2-D ray-tracing and P-wave travel time modelling and new results of P-wave travel time residuals methods and receiver function sections provide facts about the seismic structure from the surface down to 900 km depth. In the TESZ a large basin, about 125 km wide, is filled with sedimentary strata (Vp < 6.0 km s− 1) to about 20 km depth. This basin is asymmetric with its northeast margin being most abrupt. The crystalline crust under this basin is only about 20 km thick today indicating that the lithosphere of Baltica was either thinned drastically or terminated along the northeast margin of the basin. The East European craton (EEC) has a ~ 45 km thick three-layered crust. The crust of the accreted terranes to the southwest is relatively thin (~ 30 km) and similar to that found in other non-cratonal areas of Western Europe. The lower crust is relatively fast (Vp > 7.0 km s− 1) along most of the P4 profile. However, lower values to the southwest may indicate the termination of Baltica. High velocity (~ 8.35 km s− 1) uppermost mantle lies beneath the Avalonia/Variscan terranes, and may be due to rifting and/or subduction. The seismic lithosphere thickness for the EEC is about 200 km, while it is only 90 km in the Palaeozoic platform (PP). The mantle transition zone is shallower and about 30 km thicker under the EEC, which could be due to thermal conditions (lower temperature) and/or the presence of water and FeO. The result of this paper is a new compiled and integrated seismic velocity model, available in digital form down to 900 km depth (http://www.igf.fuw.edu.pl/p4-mantle), which can be used as a preliminary model of the crust and upper mantle in the TESZ area in Central Europe." @default.
• W1991325145 created "2016-06-24" @default.
• W1991325145 creator A5007939184 @default.
• W1991325145 creator A5073263992 @default.
• W1991325145 creator A5075298121 @default.
• W1991325145 creator A5085733955 @default.
• W1991325145 date "2010-01-01" @default.
• W1991325145 modified "2023-10-18" @default.
• W1991325145 title "Integrated seismic model of the crust and upper mantle of the Trans-European Suture zone between the Precambrian craton and Phanerozoic terranes in Central Europe" @default.
• W1991325145 cites W1543326455 @default.
• W1991325145 cites W1824072299 @default.
• W1991325145 cites W1968791485 @default.
• W1991325145 cites W1987958335 @default.
• W1991325145 cites W2004875655 @default.
• W1991325145 cites W2006352148 @default.
• W1991325145 cites W2007056155 @default.
• W1991325145 cites W2014490938 @default.
• W1991325145 cites W2015000331 @default.
• W1991325145 cites W2017846713 @default.
• W1991325145 cites W2018314772 @default.
• W1991325145 cites W2023602033 @default.
• W1991325145 cites W2023893845 @default.
• W1991325145 cites W2025160267 @default.
• W1991325145 cites W2025674481 @default.
• W1991325145 cites W2027934726 @default.
• W1991325145 cites W2029061251 @default.
• W1991325145 cites W2029434609 @default.
• W1991325145 cites W2031399370 @default.
• W1991325145 cites W2031458587 @default.
• W1991325145 cites W2037094469 @default.
• W1991325145 cites W2040823285 @default.
• W1991325145 cites W2043753589 @default.
• W1991325145 cites W2045040002 @default.
• W1991325145 cites W2047408998 @default.
• W1991325145 cites W2060335907 @default.
• W1991325145 cites W2064665870 @default.
• W1991325145 cites W2065461551 @default.
• W1991325145 cites W2075389126 @default.
• W1991325145 cites W2075537612 @default.
• W1991325145 cites W2078138387 @default.
• W1991325145 cites W2085516284 @default.
• W1991325145 cites W2087115873 @default.
• W1991325145 cites W2087929307 @default.
• W1991325145 cites W2098465349 @default.
• W1991325145 cites W2103113534 @default.
• W1991325145 cites W2109433936 @default.
• W1991325145 cites W2110154385 @default.
• W1991325145 cites W2125158311 @default.
• W1991325145 cites W2130631262 @default.
• W1991325145 cites W2153806527 @default.
• W1991325145 cites W2155516056 @default.
• W1991325145 cites W2170994364 @default.
• W1991325145 cites W2561898317 @default.
• W1991325145 cites W2646393 @default.
• W1991325145 cites W2790685744 @default.
• W1991325145 cites W4211228162 @default.
• W1991325145 doi "https://doi.org/10.1016/j.tecto.2009.05.002" @default.
• W1991325145 hasPublicationYear "2010" @default.
• W1991325145 type Work @default.
• W1991325145 sameAs 1991325145 @default.
• W1991325145 citedByCount "48" @default.
• W1991325145 countsByYear W19913251452012 @default.
• W1991325145 countsByYear W19913251452013 @default.
• W1991325145 countsByYear W19913251452014 @default.
• W1991325145 countsByYear W19913251452015 @default.
• W1991325145 countsByYear W19913251452016 @default.
• W1991325145 countsByYear W19913251452017 @default.
• W1991325145 countsByYear W19913251452018 @default.
• W1991325145 countsByYear W19913251452019 @default.
• W1991325145 countsByYear W19913251452020 @default.
• W1991325145 countsByYear W19913251452021 @default.
• W1991325145 countsByYear W19913251452022 @default.
• W1991325145 countsByYear W19913251452023 @default.
• W1991325145 crossrefType "journal-article" @default.
• W1991325145 hasAuthorship W1991325145A5007939184 @default.
• W1991325145 hasAuthorship W1991325145A5073263992 @default.
• W1991325145 hasAuthorship W1991325145A5075298121 @default.
• W1991325145 hasAuthorship W1991325145A5085733955 @default.
• W1991325145 hasConcept C105702510 @default.
• W1991325145 hasConcept C127313418 @default.
• W1991325145 hasConcept C13495919 @default.
• W1991325145 hasConcept C147717901 @default.
• W1991325145 hasConcept C150999391 @default.
• W1991325145 hasConcept C151730666 @default.
• W1991325145 hasConcept C165205528 @default.
• W1991325145 hasConcept C16942324 @default.
• W1991325145 hasConcept C173776410 @default.
• W1991325145 hasConcept C2776698055 @default.
• W1991325145 hasConcept C2777040169 @default.
• W1991325145 hasConcept C2777327002 @default.
• W1991325145 hasConcept C2780356177 @default.
• W1991325145 hasConcept C67236022 @default.
• W1991325145 hasConcept C71924100 @default.
• W1991325145 hasConcept C77928131 @default.
• W1991325145 hasConcept C8058405 @default.
• W1991325145 hasConcept C91442348 @default.
• W1991325145 hasConceptScore W1991325145C105702510 @default.
• W1991325145 hasConceptScore W1991325145C127313418 @default.

• next