A subglacial hydrologic drainage hypothesis for silt sorting and deposition during retreat in Pine Island Bay
Late Holocene sediment deposits in Pine Island Bay, West Antarctica, are hypothesized to be linked to intensive meltwater drainage during the retreat of the paleo-Pine Island Ice Stream after the Last Glacial Maximum. The uppermost sediment units show an abrupt transition from ice-proximal debris to...
محفوظ في:
| المؤلفون الرئيسيون: | , , , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
Cambridge University Press
2019-12-01
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| سلاسل: | Annals of Glaciology |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://www.cambridge.org/core/product/identifier/S0260305519000442/type/journal_article |
| الوسوم: |
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