Haflidi Haflidason focuses on Oceanography, Geomorphology, Paleontology, Ice sheet and Glacial period. Haflidi Haflidason studied Oceanography and Tephrochronology that intersect with Preboreal. His study in Geomorphology is interdisciplinary in nature, drawing from both Continental shelf and Debris.
His research integrates issues of Radiocarbon dating and Ice core in his study of Younger Dryas. His Radiocarbon dating research includes elements of Epigravettian, Surface ocean, Remote sensing and Multi proxy. Along with Ice core, other disciplines of study including Field intensity, Calibration curve and Calibration are integrated into his research.
His primary areas of investigation include Oceanography, Paleontology, Glacial period, Geomorphology and Holocene. His Oceanography and Ice sheet, Deglaciation, Younger Dryas, Ice stream and Foraminifera investigations all form part of his Oceanography research activities. His research on Younger Dryas frequently links to adjacent areas such as Fjord.
Haflidi Haflidason focuses mostly in the field of Glacial period, narrowing it down to matters related to Physical geography and, in some cases, Arctic. As a member of one scientific family, Haflidi Haflidason mostly works in the field of Geomorphology, focusing on Continental shelf and, on occasion, Continental margin and Debris. His Holocene research is multidisciplinary, incorporating elements of Tephrochronology, Tephra, Radiocarbon dating and Paleoclimatology.
Arctic, Polar, Oceanography, Glacial period and Paleontology are his primary areas of study. His study on Arctic also encompasses disciplines like
He brings together Glacial period and Clathrate hydrate to produce work in his papers. The Paleontology study combines topics in areas such as Ridge and Peninsula. Haflidi Haflidason has included themes like Boreal, Dominance, Younger Dryas, Carex and Plant community in his Pollen study.
His main research concerns Glacial period, Polar, Physical geography, Arctic and Ridge. In his articles, Haflidi Haflidason combines various disciplines, including Glacial period and Clathrate hydrate. There are a combination of areas like Varve, Climate history, Resolution and Geomorphological mapping integrated together with his Polar study.
As part of his studies on Ridge, Haflidi Haflidason frequently links adjacent subjects like Geochemistry.
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IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP
Paula J Reimer;Edouard Bard;Alex Bayliss;J Warren Beck.
Radiocarbon (2009)
Paleoceanographic reconstructions of surface ocean conditions in the Greenland, Iceland and Norwegian seas through the last 14 ka based on diatoms
Nalân Koç;Eystein Jansen;Haflidi Haflidason.
Quaternary Science Reviews (1993)
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project
M. Canals;G. Lastras;R. Urgeles;J.L. Casamor.
Marine Geology (2004)
The Storegga Slide: architecture, geometry and slide development
Haflidi Haflidason;Hans Petter Sejrup;Atle Nygård;Jurgen Mienert.
Marine Geology (2004)
Triggering mechanisms of slope instability processes and sediment failures on continental margins: a geotechnical approach
Nabil Sultan;Pierre Cochonat;M Canals;Antonio Cattaneo.
Marine Geology (2004)
Ocean warming and gas hydrate stability on the mid-Norwegian margin at the Storegga Slide
Jürgen Mienert;Maarten Vanneste;Stefan Bünz;Karin Andreassen.
Marine and Petroleum Geology (2005)
The dating and morphometry of the Storegga Slide
Haflidi Haflidason;Reidar Lien;Hans Petter Sejrup;Carl Fredrik Forsberg;Carl Fredrik Forsberg.
Marine and Petroleum Geology (2005)
The tephrochronology of Iceland and the North Atlantic region during the Middle and Late Quaternary: a review
Haflidi Haflidason;Jon Eiriksson;Shirley Van Kreveld.
Journal of Quaternary Science (2000)
Pleistocene glacial history of the NW European continental margin
Hans Petter Sejrup;Berit Oline Hjelstuen;K.I. Torbjørn Dahlgren;Haflidi Haflidason.
Marine and Petroleum Geology (2005)
A regional 8200 cal. yr BP cooling event in northwest Europe, induced by final stages of the Laurentide ice-sheet deglaciation?
Dorthe Klitgaard-Kristensen;Hans Petter Sejrup;Haflidi Haflidason;Sigfus Johnsen.
Journal of Quaternary Science (1998)
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