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Just Published Articles
- Evidence of a full West Antarctic Ice Sheet back to the early Oligocene: insight from double dating of detrital apatites in Ross Sea sediments
Valerio Olivetti, Maria Laura Balestrieri, Federico Rossetti, Stuart N Thomson, Franco M Talarico and Massimiliano Zattin
Accepted manuscript online: 25 MAR 2015 09:36AM EST | DOI: 10.1111/ter.12153
- Critical taper behaviour and out-of-sequence thrusting on orogenic wedges - an example of the Eastern Alpine Molasse Basin
Volker Schuller, Wolfgang Frisch and Ulrich Herzog
Accepted manuscript online: 23 MAR 2015 02:25AM EST | DOI: 10.1111/ter.12152
- How bioturbation obscured the Cretaceous-Palaeogene boundary record
Laia Alegret, Francisco J. Rodríguez-Tovar and Alfred Uchman
Accepted manuscript online: 18 MAR 2015 08:51PM EST | DOI: 10.1111/ter.12151
- Does subduction polarity control metallogeny? The Mediterranean case (pages 139–146)
Paolo Nimis and Paolo Omenetto
Article first published online: 14 MAR 2015 | DOI: 10.1111/ter.12141
- Tectonically induced change in lake evolution recorded by seismites in the Eocene Green River Formation, Wyoming
Balázs Törő, Brian R. Pratt and Robin W. Renaut
Accepted manuscript online: 14 MAR 2015 02:22AM EST | DOI: 10.1111/ter.12150
The onset of glaciation in Greenland:
Large-scale glaciations in the Arctic only began about 2.7 million years ago; before that, the northern hemisphere had been largely free of ice for more than 500 million years. What factors allowed the glaciation of Greenland to begin? Steinberger et al. identify three solid-Earth processes that played an important role. Firstly, the Iceland plume was directly beneath East Greenland from about 60 to 30 million years ago. This is the likely reason why the lithosphere there even today is only about 90 km thick. More recent pulses of hot material rising through the Iceland plume could flow beneath the thin lithosphere. The most recent pulse arrived there during the past 10 million years, and uplifted East Greenland, forming high mountains. Secondly, tectonic plate motion moved Greenland northward. And thirdly, a shift in the Earth's axis termed 'True Polar Wander' had the effect of moving Greenland still further north. The combined effect was a northward shift of about 18° during the past 60 million years. Hence Greenland was only recently sufficiently far north, and its mountain tops in the east were sufficiently high, that glaciations could be initiated.
Read the full article:
The key role of global solid-Earth processes in preconditioning Greenland's glaciation since the Pliocene
Bernhard Steinberger, Wim Spakman, Peter Japsen and Trond H. Torsvik
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Caveats on tomographic images.Gillian R. Foulger, Giuliano F. Panza, Irina M. Artemieva, Ian D. Bastow, Fabio Cammarano, John R. Evans, Warren B. Hamilton, Bruce R. Julian, Michele Lustrino, Hans Thybo and Tatiana B. Yanovskaya
Local high relief at the southern margin of the Andean plateau by 9 Ma: evidence from ignimbritic valley fills and river incision. Carolina Montero-López, Manfred R. Strecker, Taylor F. Schildgen, Fernando Hongn, Silvina Guzmán, Bodo Bookhagen and Masafumi Sudo
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