FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017148175> ?p ?o ?g. }

• W2017148175 endingPage "154" @default.
• W2017148175 startingPage "126" @default.
• W2017148175 abstract "Abstract This study provides an up-to-date and comprehensive review of the Early Palaeozoic evolution of the Brabant Massif belonging to the Anglo-Brabant Deformation Belt. Situated at the southeastern side of Avalonia microplate, it is the only well-known part of the northern passive margin of the Rheic Ocean. The Cambrian–Silurian sedimentary pile is > 13 km thick, with > 9 km for the Cambrian only. The unraveling of this continuous registration reflects the successive rifting and drifting of Avalonia from the Gondwana mainland, followed by soft-collisional processes with Baltica and finally the formation of Laurussia. Based on recently established detailed stratigraphy, sedimentology and basin development, on U–Pb LA-ICP-MS analyses of igneous and detrital zircon grains along with geochemical data including Sm–Nd isotopes, a new geodynamic and palaeogeographic evolution is proposed. Brabant Megasequence 1 (lower Cambrian to lowermost Ordovician, > 9 km thick) represents an embayment of the peri-Gondwanan rift from which the Rheic Ocean has evolved. Detrital zircon ages demonstrate that the Brabant is a typical peri-Gondwanan terrane with a major Pan-African (Neoproterozoic age) and a mixed West African and Amazonian source (Palaeoproterozoic, Archaean and some Mesoproterozoic age). The transition towards the Avalonia drifting is marked by an unconformity and a short volcanic episode. The northward drift of Avalonia towards Baltica is recorded by the Megasequence 2 (Middle to Upper Ordovician, 1.3 km thick). The source for Mesoproterozoic zircons vanished, as the result of the Rheic Ocean opening and the isolation from Amazonian sources. The transition to Megasequence 3 is marked by a drastic change in palaeobathymetry and an important (sub)volcanic episode during a tectonic instability period (460–430 Ma), reflecting the Avalonia–Baltica soft docking as also shown by the reappearance of Mesoproterozoic detrital zircons, typical of Baltica. Unradiogenic Nd isotope signature (eNd − 4/− 5) and TDM model ages (1.3–1.7 Ga) for Brabant magmatic rocks indicate an old recycled component. Megasequence 3 (uppermost Ordovician to lowermost Devonian; > 3.5 km thick) includes the onset of a Silurian foreland basin that reflects the tectonic inversion of the core of the massif (Brabantian orogeny) in response to the Baltica–Avalonia–Laurentia collision. Finally, the comparison with the strikingly similar Cambrian successions of the Harlech Dome (Wales, Avalonia) and the Meguma terrane (Nova Scotia, peri-Gondwana) allows the construction of a new Early Cambrian palaeogeographic model for the whole Avalonia microplate, in which the Meguma terrane is included." @default.
• W2017148175 created "2016-06-24" @default.
• W2017148175 creator A5039858005 @default.
• W2017148175 creator A5047903297 @default.
• W2017148175 creator A5048832144 @default.
• W2017148175 creator A5049639227 @default.
• W2017148175 creator A5050983722 @default.
• W2017148175 creator A5055313905 @default.
• W2017148175 date "2012-05-01" @default.
• W2017148175 modified "2023-10-02" @default.
• W2017148175 title "The Cambrian to Devonian odyssey of the Brabant Massif within Avalonia: A review with new zircon ages, geochemistry, Sm–Nd isotopes, stratigraphy and palaeogeography" @default.
• W2017148175 cites W131462090 @default.
• W2017148175 cites W1871724464 @default.
• W2017148175 cites W1968012520 @default.
• W2017148175 cites W1970771502 @default.
• W2017148175 cites W1971376046 @default.
• W2017148175 cites W1979350315 @default.
• W2017148175 cites W1979982652 @default.
• W2017148175 cites W1980863739 @default.
• W2017148175 cites W1990748926 @default.
• W2017148175 cites W1994855356 @default.
• W2017148175 cites W1997266026 @default.
• W2017148175 cites W2001218033 @default.
• W2017148175 cites W2003703699 @default.
• W2017148175 cites W2006391679 @default.
• W2017148175 cites W2007105153 @default.
• W2017148175 cites W2011896746 @default.
• W2017148175 cites W2012383753 @default.
• W2017148175 cites W2017042976 @default.
• W2017148175 cites W2019937834 @default.
• W2017148175 cites W2023424507 @default.
• W2017148175 cites W2024089139 @default.
• W2017148175 cites W2026245988 @default.
• W2017148175 cites W2028313440 @default.
• W2017148175 cites W2029061251 @default.
• W2017148175 cites W2029174554 @default.
• W2017148175 cites W2037908389 @default.
• W2017148175 cites W2039100744 @default.
• W2017148175 cites W2040029696 @default.
• W2017148175 cites W2041828123 @default.
• W2017148175 cites W2046954615 @default.
• W2017148175 cites W2047364329 @default.
• W2017148175 cites W2050285694 @default.
• W2017148175 cites W2052663957 @default.
• W2017148175 cites W2053593932 @default.
• W2017148175 cites W2055191285 @default.
• W2017148175 cites W2059356468 @default.
• W2017148175 cites W2060541428 @default.
• W2017148175 cites W2068531798 @default.
• W2017148175 cites W2070142384 @default.
• W2017148175 cites W2073451667 @default.
• W2017148175 cites W2073942336 @default.
• W2017148175 cites W2082082808 @default.
• W2017148175 cites W2084714346 @default.
• W2017148175 cites W2088223235 @default.
• W2017148175 cites W2089950189 @default.
• W2017148175 cites W2094758778 @default.
• W2017148175 cites W2095878716 @default.
• W2017148175 cites W2097394294 @default.
• W2017148175 cites W2101718819 @default.
• W2017148175 cites W2103932516 @default.
• W2017148175 cites W2108259914 @default.
• W2017148175 cites W2117487772 @default.
• W2017148175 cites W2118768659 @default.
• W2017148175 cites W2121810349 @default.
• W2017148175 cites W2122743079 @default.
• W2017148175 cites W2128956731 @default.
• W2017148175 cites W2133378225 @default.
• W2017148175 cites W2150913154 @default.
• W2017148175 cites W2155843218 @default.
• W2017148175 cites W2158179275 @default.
• W2017148175 cites W2164468447 @default.
• W2017148175 cites W2168969287 @default.
• W2017148175 cites W2319100471 @default.
• W2017148175 cites W4251816327 @default.
• W2017148175 cites W76373824 @default.
• W2017148175 doi "https://doi.org/10.1016/j.earscirev.2012.02.007" @default.
• W2017148175 hasPublicationYear "2012" @default.
• W2017148175 type Work @default.
• W2017148175 sameAs 2017148175 @default.
• W2017148175 citedByCount "94" @default.
• W2017148175 countsByYear W20171481752012 @default.
• W2017148175 countsByYear W20171481752013 @default.
• W2017148175 countsByYear W20171481752014 @default.
• W2017148175 countsByYear W20171481752015 @default.
• W2017148175 countsByYear W20171481752016 @default.
• W2017148175 countsByYear W20171481752017 @default.
• W2017148175 countsByYear W20171481752018 @default.
• W2017148175 countsByYear W20171481752019 @default.
• W2017148175 countsByYear W20171481752020 @default.
• W2017148175 countsByYear W20171481752021 @default.
• W2017148175 countsByYear W20171481752022 @default.
• W2017148175 countsByYear W20171481752023 @default.
• W2017148175 crossrefType "journal-article" @default.
• W2017148175 hasAuthorship W2017148175A5039858005 @default.
• W2017148175 hasAuthorship W2017148175A5047903297 @default.
• W2017148175 hasAuthorship W2017148175A5048832144 @default.
• W2017148175 hasAuthorship W2017148175A5049639227 @default.

• next