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Just Published Articles
- Low melting temperature for calcite at 1000 bars on the join CaCO3-H2O – some geological implications
Cyril Durand, Lukas P. Baumgartner and Didier Marquer
Article first published online: 6 JUL 2015 | DOI: 10.1111/ter.12168
- A metamorphic perspective on foreland flexure during intraplate orogeny: evidence for the involvement of weak lithosphere
Alec K. Walsh, Martin Hand and David E. Kelsey
Article first published online: 30 JUN 2015 | DOI: 10.1111/ter.12164
- Regional provenance from southwestern Colombia fore-arc and intra-arc basins: implications for Middle to Late Miocene orogeny in the Northern Andes
Sebastián Echeverri, Agustín Cardona, Andrés Pardo, Gaspar Monsalve, Victor A. Valencia, Carlos Borrero, Sebastián Rosero and Sergio López
Article first published online: 29 JUN 2015 | DOI: 10.1111/ter.12167
- Multi-scale stratigraphic forward modelling of the Surat Basin for geological storage of CO2
Johannes J. Ravestein, Cedric M. Griffiths, Chris P. Dyt and Karsten Michael
Article first published online: 29 JUN 2015 | DOI: 10.1111/ter.12166
- Modelling the long-term deformation of the sedimentary substrate of Mt. Etna volcano (Italy)
Salvatore Scudero, Giorgio De Guidi, Sebastiano Imposa and Gilda Currenti
Article first published online: 29 JUN 2015 | DOI: 10.1111/ter.12165
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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This article, written by Professor Stuart Lane, editor of Earth Surface Processes and Landforms, provides excellent guidelines for Chinese authors. The article has been translated into local language for easy reading and comprehension.
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