Progressive ductile shearing during till accretion within the deforming bed of a palaeo-ice stream

Emrys Phillips, Matteo Spagnolo, Alasdair C. J. Pilmer, Brice R. Rea, Jan A. Piotrowski, Jeremy C. Ely, Simon Carr

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

This paper presents the results of a detailed microstructural study of a thick till formed beneath the Weichselian (Devensian) Odra palaeo-ice stream, west of Środa Wielkopolska, Poland. This SE-flowing ice stream was one of a number of corridors of faster flowing ice which drained the Scandinavian Ice Sheet in the Baltic region. Macroscopically, the massive, laterally extensive till which formed the bed of this ice stream lacks any obvious evidence of glaciotectonism (thrusting, folding). However, microscale analysis reveals that bed deformation was dominated by foliation development, recording progressive ductile shearing within a subhorizontal subglacial shear zone. Five successive generations of clast microfabric (S1 to S5) have been identified defining a set of up-ice and down-ice dipping Riedel shears, as well as a subhorizontal shear foliation coplanar to the ice-bed interface. Cross-cutting relationships between the shear fabrics record temporal changes in the style of deformation during this progressive shear event. Kinematic indicators (S-C and ECC-type fabrics) within the till indicate a consistent SE-directed shear sense, in agreement with the regional ice flow pattern. A model of bed deformation involving incremental progressive simple shear during till accretion is proposed. The relative age of this deformation was diachronous becoming progressively younger upwards, compatible with subglacial shearing having accompanied till accretion at the top of the deforming bed. Variation in the relative intensity of the microfabrics records changes in the magnitude of the cumulative strain imposed on the till and the degree of coupling between the ice and underlying bed during fast ice flow.
Original languageEnglish
Pages (from-to)1-23
Number of pages23
JournalQuaternary Science Reviews
Volume193
Early online date2 Jul 2018
DOIs
Publication statusPublished - 1 Aug 2018

Fingerprint

Baltic region
ice stream
Poland
recording
ice
accretion
shear stress
event
lack
evidence
ice flow
foliation
temporal record
Scandinavian Ice Sheet
Devensian
Weichselian
flow pattern
clast
folding
shear zone

Keywords

  • micromorphology
  • glacier bed deformation
  • ductile shearing
  • foliation development
  • palaeo-ice stream

Cite this

Progressive ductile shearing during till accretion within the deforming bed of a palaeo-ice stream. / Phillips, Emrys; Spagnolo, Matteo; Pilmer, Alasdair C. J.; Rea, Brice R.; Piotrowski, Jan A.; Ely, Jeremy C.; Carr, Simon.

In: Quaternary Science Reviews, Vol. 193, 01.08.2018, p. 1-23.

Research output: Contribution to journalArticle

Phillips, Emrys ; Spagnolo, Matteo ; Pilmer, Alasdair C. J. ; Rea, Brice R. ; Piotrowski, Jan A. ; Ely, Jeremy C. ; Carr, Simon. / Progressive ductile shearing during till accretion within the deforming bed of a palaeo-ice stream. In: Quaternary Science Reviews. 2018 ; Vol. 193. pp. 1-23.
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abstract = "This paper presents the results of a detailed microstructural study of a thick till formed beneath the Weichselian (Devensian) Odra palaeo-ice stream, west of Środa Wielkopolska, Poland. This SE-flowing ice stream was one of a number of corridors of faster flowing ice which drained the Scandinavian Ice Sheet in the Baltic region. Macroscopically, the massive, laterally extensive till which formed the bed of this ice stream lacks any obvious evidence of glaciotectonism (thrusting, folding). However, microscale analysis reveals that bed deformation was dominated by foliation development, recording progressive ductile shearing within a subhorizontal subglacial shear zone. Five successive generations of clast microfabric (S1 to S5) have been identified defining a set of up-ice and down-ice dipping Riedel shears, as well as a subhorizontal shear foliation coplanar to the ice-bed interface. Cross-cutting relationships between the shear fabrics record temporal changes in the style of deformation during this progressive shear event. Kinematic indicators (S-C and ECC-type fabrics) within the till indicate a consistent SE-directed shear sense, in agreement with the regional ice flow pattern. A model of bed deformation involving incremental progressive simple shear during till accretion is proposed. The relative age of this deformation was diachronous becoming progressively younger upwards, compatible with subglacial shearing having accompanied till accretion at the top of the deforming bed. Variation in the relative intensity of the microfabrics records changes in the magnitude of the cumulative strain imposed on the till and the degree of coupling between the ice and underlying bed during fast ice flow.",
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author = "Emrys Phillips and Matteo Spagnolo and Pilmer, {Alasdair C. J.} and Rea, {Brice R.} and Piotrowski, {Jan A.} and Ely, {Jeremy C.} and Simon Carr",
note = "The authors would like to thank various colleagues for numerous discussions on the nature of glacier bed deformation over the years, in particular Dave Evans, Jaap van der Meer, Jonathan Lee, Clive Auton, Jon Merritt, Chris Clark, Chris Stokes, Wojciech Wysota, Iza Szuman and Adriano Ribolini. Adrian Palmer (Royal Holloway University of London) is thanked for his expertise in making the thin sections. David J.A. Evans and one anonymous reviewer are thanked for their constructive reviews of this paper. ERP publishes with the permission of the Executive Director of the British Geological Survey, Natural Environment Research Council. The sampling and thin section preparation was funded by the NERC NE/J004766/1 grant awarded to MS. Appendix A. Supplementary data Supplementary data related to this article can be found at https://doi.org/10.1016/j.quascirev.2018.06.009.",
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AU - Piotrowski, Jan A.

AU - Ely, Jeremy C.

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N1 - The authors would like to thank various colleagues for numerous discussions on the nature of glacier bed deformation over the years, in particular Dave Evans, Jaap van der Meer, Jonathan Lee, Clive Auton, Jon Merritt, Chris Clark, Chris Stokes, Wojciech Wysota, Iza Szuman and Adriano Ribolini. Adrian Palmer (Royal Holloway University of London) is thanked for his expertise in making the thin sections. David J.A. Evans and one anonymous reviewer are thanked for their constructive reviews of this paper. ERP publishes with the permission of the Executive Director of the British Geological Survey, Natural Environment Research Council. The sampling and thin section preparation was funded by the NERC NE/J004766/1 grant awarded to MS. Appendix A. Supplementary data Supplementary data related to this article can be found at https://doi.org/10.1016/j.quascirev.2018.06.009.

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N2 - This paper presents the results of a detailed microstructural study of a thick till formed beneath the Weichselian (Devensian) Odra palaeo-ice stream, west of Środa Wielkopolska, Poland. This SE-flowing ice stream was one of a number of corridors of faster flowing ice which drained the Scandinavian Ice Sheet in the Baltic region. Macroscopically, the massive, laterally extensive till which formed the bed of this ice stream lacks any obvious evidence of glaciotectonism (thrusting, folding). However, microscale analysis reveals that bed deformation was dominated by foliation development, recording progressive ductile shearing within a subhorizontal subglacial shear zone. Five successive generations of clast microfabric (S1 to S5) have been identified defining a set of up-ice and down-ice dipping Riedel shears, as well as a subhorizontal shear foliation coplanar to the ice-bed interface. Cross-cutting relationships between the shear fabrics record temporal changes in the style of deformation during this progressive shear event. Kinematic indicators (S-C and ECC-type fabrics) within the till indicate a consistent SE-directed shear sense, in agreement with the regional ice flow pattern. A model of bed deformation involving incremental progressive simple shear during till accretion is proposed. The relative age of this deformation was diachronous becoming progressively younger upwards, compatible with subglacial shearing having accompanied till accretion at the top of the deforming bed. Variation in the relative intensity of the microfabrics records changes in the magnitude of the cumulative strain imposed on the till and the degree of coupling between the ice and underlying bed during fast ice flow.

AB - This paper presents the results of a detailed microstructural study of a thick till formed beneath the Weichselian (Devensian) Odra palaeo-ice stream, west of Środa Wielkopolska, Poland. This SE-flowing ice stream was one of a number of corridors of faster flowing ice which drained the Scandinavian Ice Sheet in the Baltic region. Macroscopically, the massive, laterally extensive till which formed the bed of this ice stream lacks any obvious evidence of glaciotectonism (thrusting, folding). However, microscale analysis reveals that bed deformation was dominated by foliation development, recording progressive ductile shearing within a subhorizontal subglacial shear zone. Five successive generations of clast microfabric (S1 to S5) have been identified defining a set of up-ice and down-ice dipping Riedel shears, as well as a subhorizontal shear foliation coplanar to the ice-bed interface. Cross-cutting relationships between the shear fabrics record temporal changes in the style of deformation during this progressive shear event. Kinematic indicators (S-C and ECC-type fabrics) within the till indicate a consistent SE-directed shear sense, in agreement with the regional ice flow pattern. A model of bed deformation involving incremental progressive simple shear during till accretion is proposed. The relative age of this deformation was diachronous becoming progressively younger upwards, compatible with subglacial shearing having accompanied till accretion at the top of the deforming bed. Variation in the relative intensity of the microfabrics records changes in the magnitude of the cumulative strain imposed on the till and the degree of coupling between the ice and underlying bed during fast ice flow.

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