Seafloor geomorphology of western Antarctic Peninsula bays: a signature of ice flow behaviour
Glacial geomorphology is used in Antarctica to reconstruct ice advance during the Last Glacial Maximum and subsequent retreat across the continental shelf. Analogous geomorphic assemblages are found in glaciated fjords and are used to interpret the glacial history and glacial dynamics in those ar...
| الحاوية / القاعدة: | The Cryosphere |
|---|---|
| المؤلفون الرئيسيون: | , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Copernicus Publications
2018-01-01
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| الوصول للمادة أونلاين: | https://www.the-cryosphere.net/12/205/2018/tc-12-205-2018.pdf |