Stratified glacimarine basin-fills in West Greenland fjords

Ó Cofaigh, C.; Hogan, K.A. ORCID: https://orcid.org/0000-0002-1256-8010; Dowdeswell, J.A.; Streuff, K.. 2016 Stratified glacimarine basin-fills in West Greenland fjords. In: Dowdeswell, J.A.; Canals, M.; Jakobsson, M.; Todd, B.J.; Dowdeswell, E.K.; Hogan, K.A., (eds.) Atlas of submarine glacial landforms: modern, Quaternary and ancient. London, Geological Society of London, 99-100. (Geological Society Memoir, 46).

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Official URL: http://mem.lyellcollection.org/content/46/1/99.sho...

Abstract/Summary

Acoustically stratified sediments that infill glacially eroded bedrock basins are common in fjords (Seramur et al. 1997; Gilbert et al. 1998; Hogan et al. 2012; Dowdeswell & Vasquez 2013). Internally, such stratified sediments are often characterized by relatively smooth reflections that parallel the seafloor. Sills between basins usually comprise bedrock, sometimes covered by a thin veneer of glacimarine sediment and/or till. Fjords in West Greenland, including Rink Fjord and Vaigat, contain bedrock basins infilled by acoustically stratified sediment (Fig. 1). The basin fills are a product of rain-out from turbid meltwater plumes, probably supplemented by iceberg-rafting and downslope resedimentation.

Item Type:	Publication - Book Section
Digital Object Identifier (DOI):	https://doi.org/10.1144/M46.83
Programmes:	BAS Programmes > BAS Programmes 2015 > Palaeo-Environments, Ice Sheets and Climate Change
ISBN:	9781786202680
Date made live:	04 Jan 2017 14:43 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/515680

Item Type:

Publication - Book Section

Digital Object Identifier (DOI):

https://doi.org/10.1144/M46.83

Programmes:

BAS Programmes > BAS Programmes 2015 > Palaeo-Environments, Ice Sheets and Climate Change

ISBN:

9781786202680

Date made live:

04 Jan 2017 14:43 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/515680