J
Jaap J.M. van der Meer
Researcher at Queen Mary University of London
Publications - 48
Citations - 2563
Jaap J.M. van der Meer is an academic researcher from Queen Mary University of London. The author has contributed to research in topics: Ice sheet & Glacier. The author has an hindex of 26, co-authored 48 publications receiving 2414 citations. Previous affiliations of Jaap J.M. van der Meer include University of London & University of Amsterdam.
Papers
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Journal ArticleDOI
Orbitally induced oscillations in the East Antarctic ice sheet at the Oligocene/Miocene boundary
Tim R Naish,Ken J. Woolfe,Peter Barrett,Gary S. Wilson,C. Atkins,Steven M Bohaty,C. Bücker,M. Claps,Fred Davey,Gavin B. Dunbar,Gavin B. Dunbar,Alistair Dunn,Christopher R. Fielding,Fabio Florindo,Fabio Florindo,M. J. Hannah,David M. Harwood,Stuart Henrys,Lawrence A. Krissek,M. Lavelle,Jaap J.M. van der Meer,Jaap J.M. van der Meer,William C. McIntosh,Frank Niessen,Sandra Passchier,Ross D. Powell,Andrew P. Roberts,Leonardo Sagnotti,Reed P. Scherer,C Percy Strong,Franco M Talarico,Kenneth L. Verosub,Giuliana Villa,David K. Watkins,P.N. Webb,Thomas Wonik +35 more
TL;DR: Sediment data from shallow marine cores in the western Ross Sea are presented that exhibit well dated cyclic variations, and which link the extent of the East Antarctic ice sheet directly to orbital cycles during the Oligocene/Miocene transition, suggesting that orbital influences at the frequencies of obliquity and eccentricity controlled the oscillations of the ice margin at that time.
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Microscopic evidence of subglacial deformation
TL;DR: A review of microscopic evidence for subglacial deformation is given in this article, where a case where deformation could be established macroscopically, then traces the microscopic features through planar and rotational movements, which are described and separated accordingly.
Journal ArticleDOI
Subglacial till: the deforming glacier bed
TL;DR: In this paper, the deforming glacier bed has been used as a framework for discussing tills and their properties, and this (tectonic) concept is irreconcilable with the existing (depositional) till classification scheme.
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Till—as a glacial “tectomict”, its internal architecture, and the development of a “typing” method for till differentiation
TL;DR: In this paper, a new term better describes tills as glacial 'tectomicts' and a statistical method is introduced that permits differentiation of tills from other diamictons.
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Clastic dykes in over-consolidated tills: evidence for subglacial hydrofracturing at Killiney Bay, eastern Ireland
TL;DR: A swarm of vertical gravel-filled dykes up to 6 m high and several decimetres wide, cut through an over-consolidated till at Killiney Bay as mentioned in this paper.