Quantitative bounds on morphodynamics and implications for reading the sedimentary record
Sedimentary rocks are the archives of environmental conditions and ancient planetary surface processes that led to their formation. Reconstructions of Earth’s past surface behaviour from the physical sedimentary record remain controversial, however, in part because we lack a quantitative framework t...
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Veröffentlicht in: | Nature communications 2014-02, Vol.5 (1), p.3298-3298, Article 3298 |
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