The spatial and temporal distribution of grain-size breaks in turbidites
ABSTRACT Grain‐size breaks are surfaces where abrupt changes in grain size occur vertically within deposits. Grain‐size breaks are common features in turbidites around the world, including ancient and modern systems. Despite their widespread occurrence, grain‐size breaks have been regarded as except...
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Veröffentlicht in: | Sedimentology 2014-06, Vol.61 (4), p.1120-1156 |
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