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Just Published Articles
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Arsenio Muñoz, Miguel Bartolomé, Alicia Muñoz, Carlos Sancho, Ana Moreno, John C. Hellstrom, M.Cinta Osácar and Isabel Cacho
Accepted manuscript online: 20 MAY 2015 10:49PM EST | DOI: 10.1111/ter.12160
- Superposition of burial and hydrothermal events: post-Variscan thermal evolution of the Erzgebirge, Germany
Reinhard Wolff, István Dunkl, Jan-M Lange, Christian Tonk, Thomas Voigt and Hilmar von Eynatten
Accepted manuscript online: 16 MAY 2015 12:16AM EST | DOI: 10.1111/ter.12159
- Isotopically diverse rhyolites coeval with the Columbia River Flood Basalts: evidence for mantle plume interaction with the continental crust
Dylan P. Colón, Ilya N. Bindeman, Richard A. Stern and Chris M. Fisher
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Accepted manuscript online: 13 MAY 2015 06:20AM EST | DOI: 10.1111/ter.12158
- Ancient mantle lithosphere beneath the Khanka massif in the Russian Far East: in situ Re-Os evidence
Kuo-Lung Wang, Vladimir Prikhodko, Suzanne Y. O'Reilly, William L. Griffin, Norman J. Pearson, Victor Kovach, Yoshiyuki Iizuka and Yu-Hsian Chien
Accepted manuscript online: 8 MAY 2015 02:56AM EST | DOI: 10.1111/ter.12157
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
The following articles are among the most popular published in Terra Nova over the last year:
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
Advice for Chinese Authors
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