Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Bjørn A. Lundschien"'
Publikováno v:
Polar Research, Vol 43, Pp 1-20 (2024)
Upper Triassic (Carnian) sandstones of the De Geerdalen Formation cored south of the island of Kvitøya (80°N), north-easternmost Svalbard, are described in terms of sedimentary facies and petrography and compared regionally in the northern Barents
Externí odkaz:
https://doaj.org/article/8016c0dddc8143f09e918bf6c7ea0df4
Autor:
Frøydis Eide, Johne Landa, Gunn Mangerud, Bjørn Anders Lundschien, Lars Haug Holen, Niall W. Paterson
Publikováno v:
Palynology. 43:53-75
Four stratigraphic cores (7533/2-U-1, 2-U-2, 3-U-7 and 7534/4-U-1) drilled in the Sentralbanken High provide important reference sections for the Upper Triassic succession in the northern Barents Sea. The cores span the De Geerdalen, Flatsalen and Sv
Autor:
Holly J. Stein, Bernard Bingen, Guangping Xu, Atle Mørk, Derek L. Schutt, Bjørn Anders Lundschien, Jorunn Os Vigran, Judith L. Hannah
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 395:222-232
The Triassic Period is bracketed by two of the ‘big five’ Phanerozoic mass extinctions. Though long viewed as a period of climatic stability, emerging data suggest multiple climatic swings and at least one severe ecological crisis. Linking these
Publikováno v:
Marine and Petroleum Geology. 27:1448-1475
A sequence stratigraphic framework of the Triassic on the Norwegian Barents shelf is presented. The Triassic succession was subdivided into five second-order sequences based on facies analysis of 2D seismic data constrained by well data. The sequence
Publikováno v:
Polar Research. 27:318-338
The interpretation of an unpublished data set of shallow stratigraphic cores and deep, seismic profiles from the northern Barents Shelf has provided new information about the Middle and Late Triassic development of the Barents Shelf and Svalbard. At
Autor:
Claus Beyer, Bjørn Anders Lundschien
Publisher Summary This chapter provides an overview on magnetostratigraphy. It is an important tool for the chronostratigraphical subdivision and dating of sedimentary sequences that are otherwise difficult to correlate and date because of the lack o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b98041b149366a5ab261c19dda00bb8
https://doi.org/10.1016/b978-044450611-5/50004-0
https://doi.org/10.1016/b978-044450611-5/50004-0