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Publikováno v:
Tullius, D N, Leier, A L, Galloway, J M, Embry, A F & Pedersen, P K 2014, ' Sedimentology and stratigraphy of the Lower Cretaceous Isachsen Formation : Ellef Ringnes Island, Sverdrup Basin, Canadian Arctic Archipelago ', Marine and Petroleum Geology, vol. 57, pp. 135-151 . https://doi.org/10.1016/j.marpetgeo.2014.05.018
The Lower Cretaceous Isachsen Formation is a widespread, siliciclastic succession up to 1.4 km thick that records the northwestward progradation of fluvio-deltaic environments into the Sverdrup Basin in the Canadian Arctic. Although the Isachsen Form
Autor:
Graeme T. Swindles, Carol A. Evenchick, Dylan N. Tullius, Ashton F. Embry, Thomas Hadlari, Jennifer M. Galloway
Quantitative palynology of the marginal marine and deltaic-fluvial Isachsen Formation of the Sverdrup Basin, Canadian Arctic, provides insight into high latitude climate during much of the Early Cretaceous (Valanginian to early Aptian). Detrended Cor
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::28ba979efd9bc79173fa814f1b09abfc
https://eprints.whiterose.ac.uk/90436/1/YCRES-D-14-00206R1_revision_submitted.pdf
https://eprints.whiterose.ac.uk/90436/1/YCRES-D-14-00206R1_revision_submitted.pdf