Carbonate slope re‐sedimentation in a tectonically‐active setting (Western Sicily Cretaceous Escarpment, Italy)
Tectonic processes are widely considered as a mechanism causing carbonate platform margin instabilities leading to the emplacement of mass transport deposits and calciturbidites. However, only few examples establishing a clear link between tectonics and re‐sedimentation processes are known from the...
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Published in | Sedimentology Vol. 67; no. 5; pp. 2360 - 2391 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Madrid
Wiley Subscription Services, Inc
01.08.2020
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Subjects | |
Online Access | Get full text |
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