Quantitative bounds on morphodynamics and implications for reading the sedimentary record.
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The exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, ChinaTime scale bias in erosion rates of glaciated landscapes.Autogenic geomorphic processes determine the resolution and fidelity of terrestrial paleoclimate recordsPhysical theory for near-bed turbulent particle suspension capacityBedform spurs: a result of a trailing helical vortex wake
P2860
Quantitative bounds on morphodynamics and implications for reading the sedimentary record.
description
2014 nî lūn-bûn
@nan
2014 թուականի Փետրուարին հրատարակուած գիտական յօդուած
@hyw
2014 թվականի փետրվարին հրատարակված գիտական հոդված
@hy
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
name
Quantitative bounds on morphod ...... eading the sedimentary record.
@ast
Quantitative bounds on morphod ...... eading the sedimentary record.
@en
type
label
Quantitative bounds on morphod ...... eading the sedimentary record.
@ast
Quantitative bounds on morphod ...... eading the sedimentary record.
@en
prefLabel
Quantitative bounds on morphod ...... eading the sedimentary record.
@ast
Quantitative bounds on morphod ...... eading the sedimentary record.
@en
P2093
P2860
P356
P1476
Quantitative bounds on morphod ...... eading the sedimentary record.
@en
P2093
Brandon McElroy
Michael P Lamb
Vamsi Ganti
P2860
P2888
P356
10.1038/NCOMMS4298
P407
P577
2014-02-28T00:00:00Z
P6179
1026493050