An origin for laminated glacimarine sediments through sea‐ice build‐up and suppressed iceberg rafting
Laminated glacimarine sediments are observed in visual core logs and x‐radiographs from Scoresby Sund and Nansen Fjord, east Greenland. They are mostly underlain and overlain by massive or stratified glacimarine diamicton (Dmm or Dms), which is a product of iceberg delivery of heterogeneous debris a...
Published in: | Sedimentology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2000
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Subjects: | |
Online Access: | http://dx.doi.org/10.1046/j.1365-3091.2000.00306.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3091.2000.00306.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3091.2000.00306.x |