FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3088973336> ?p ?o ?g. }

• W3088973336 endingPage "104717" @default.
• W3088973336 startingPage "104717" @default.
• W3088973336 abstract "Transform margins represent strike-slip type of plate boundaries that form during continental breakup and initial ocean opening. They are often characterized by margin-parallel highs with exposed pre- and syn-rift sequences. The Vøring Transform Margin, offshore mid-Norway, initiated in the earliest Eocene during the opening of the NE Atlantic. Here, 2D seismic reflection data reveal a transform margin high, the Mímir High. The western flank of this undrilled structure is a kilometer-high escarpment where seismic reflections of pre-breakup age are truncated at the seafloor. The aim of this study was to recover seabed rock samples from the outcropping or shallowly buried sedimentary sequences to provide a geological tie to the regional seismic framework, thereby constraining the basin history and tectono-stratigraphic development. Seabed samples were successfully collected from 14 gravity core and Selcore stations and 10 ROV (remotely operated vehicle) sites along a 750 m high sampling profile, recovering clay, shales, sandstones and glacial dropstones. Biostratigraphy results revealed that the ages of the sedimentary rocks follow the stratigraphic order predicted by the initial seismic interpretation, with Upper Cretaceous sediments at the base and lower Eocene sediments at the top. The integrated interpretation shows that the Mímir High area, including parts of the outer Vøring and Møre basins and the proto-Jan Mayen Microplate Complex, were characterized by the deposition of late Campanian to early Maastrichtian, near coastal and shale-dominated sequences with poor source rock qualities. The early Paleocene samples indicate deep marine conditions that abruptly ended by rapid uplift of the Mímir High in the earliest Eocene. Finally, a reworked Pliensbachian palynomorph assemblage in potential early Eocene strata indicate the presence of exposed Mesozoic sequences in the vicinity of the Mímir High. We argue that some of the lower Eocene sediments where deposited within a hypothetical drainage system sourced from Greenland (Traill Ø or Jameson Land) and/or from the Jan Mayen Ridge prior to continental separation, and not the result of recent ice-rafting." @default.
• W3088973336 created "2020-10-01" @default.
• W3088973336 creator A5003749343 @default.
• W3088973336 creator A5005137860 @default.
• W3088973336 creator A5014176009 @default.
• W3088973336 creator A5033578838 @default.
• W3088973336 creator A5035861435 @default.
• W3088973336 creator A5041880221 @default.
• W3088973336 creator A5048224709 @default.
• W3088973336 creator A5058853922 @default.
• W3088973336 creator A5061496683 @default.
• W3088973336 creator A5067450588 @default.
• W3088973336 creator A5068105372 @default.
• W3088973336 creator A5077430398 @default.
• W3088973336 creator A5080457251 @default.
• W3088973336 creator A5088672263 @default.
• W3088973336 date "2020-12-01" @default.
• W3088973336 modified "2023-10-18" @default.
• W3088973336 title "Upper Cretaceous-Paleogene stratigraphy and development of the Mímir High, Vøring Transform Margin, Norwegian Sea" @default.
• W3088973336 cites W1432316040 @default.
• W3088973336 cites W1481881169 @default.
• W3088973336 cites W1583267848 @default.
• W3088973336 cites W171697594 @default.
• W3088973336 cites W1828793079 @default.
• W3088973336 cites W1965078451 @default.
• W3088973336 cites W1965161592 @default.
• W3088973336 cites W1970319070 @default.
• W3088973336 cites W1972044496 @default.
• W3088973336 cites W1990919062 @default.
• W3088973336 cites W1993511896 @default.
• W3088973336 cites W2004593060 @default.
• W3088973336 cites W2012373503 @default.
• W3088973336 cites W2020414925 @default.
• W3088973336 cites W2023413705 @default.
• W3088973336 cites W2027335674 @default.
• W3088973336 cites W2035171494 @default.
• W3088973336 cites W2050909471 @default.
• W3088973336 cites W2051884363 @default.
• W3088973336 cites W2058772564 @default.
• W3088973336 cites W2064484532 @default.
• W3088973336 cites W2070357922 @default.
• W3088973336 cites W2072941962 @default.
• W3088973336 cites W2082467995 @default.
• W3088973336 cites W2084711994 @default.
• W3088973336 cites W2101676819 @default.
• W3088973336 cites W2103523218 @default.
• W3088973336 cites W2108162452 @default.
• W3088973336 cites W2112392524 @default.
• W3088973336 cites W2123915079 @default.
• W3088973336 cites W2129244095 @default.
• W3088973336 cites W2132204027 @default.
• W3088973336 cites W2141082108 @default.
• W3088973336 cites W2144278239 @default.
• W3088973336 cites W2160180808 @default.
• W3088973336 cites W2162423032 @default.
• W3088973336 cites W2163549037 @default.
• W3088973336 cites W2167804396 @default.
• W3088973336 cites W2169726443 @default.
• W3088973336 cites W2174799382 @default.
• W3088973336 cites W2182644802 @default.
• W3088973336 cites W2295415946 @default.
• W3088973336 cites W2405104292 @default.
• W3088973336 cites W2429577639 @default.
• W3088973336 cites W2438926368 @default.
• W3088973336 cites W2473954210 @default.
• W3088973336 cites W2520604931 @default.
• W3088973336 cites W2596279950 @default.
• W3088973336 cites W2612087402 @default.
• W3088973336 cites W2765469635 @default.
• W3088973336 cites W2783077802 @default.
• W3088973336 cites W2801574644 @default.
• W3088973336 cites W2888914634 @default.
• W3088973336 cites W2939242780 @default.
• W3088973336 cites W2971486618 @default.
• W3088973336 cites W3004463001 @default.
• W3088973336 cites W3032307867 @default.
• W3088973336 doi "https://doi.org/10.1016/j.marpetgeo.2020.104717" @default.
• W3088973336 hasPublicationYear "2020" @default.
• W3088973336 type Work @default.
• W3088973336 sameAs 3088973336 @default.
• W3088973336 citedByCount "10" @default.
• W3088973336 countsByYear W30889733362021 @default.
• W3088973336 countsByYear W30889733362022 @default.
• W3088973336 countsByYear W30889733362023 @default.
• W3088973336 crossrefType "journal-article" @default.
• W3088973336 hasAuthorship W3088973336A5003749343 @default.
• W3088973336 hasAuthorship W3088973336A5005137860 @default.
• W3088973336 hasAuthorship W3088973336A5014176009 @default.
• W3088973336 hasAuthorship W3088973336A5033578838 @default.
• W3088973336 hasAuthorship W3088973336A5035861435 @default.
• W3088973336 hasAuthorship W3088973336A5041880221 @default.
• W3088973336 hasAuthorship W3088973336A5048224709 @default.
• W3088973336 hasAuthorship W3088973336A5058853922 @default.
• W3088973336 hasAuthorship W3088973336A5061496683 @default.
• W3088973336 hasAuthorship W3088973336A5067450588 @default.
• W3088973336 hasAuthorship W3088973336A5068105372 @default.
• W3088973336 hasAuthorship W3088973336A5077430398 @default.
• W3088973336 hasAuthorship W3088973336A5080457251 @default.

• next