TY - JOUR

T1 - Microstructures and microshears as proxy for strain in subglacial diamicts

T2 - Implications for basal till formation

AU - Larsen, Nicolaj K.

AU - Piotrowski, Jan A.

AU - Christiansen, Frits

PY - 2006

Y1 - 2006

N2 - Ring-shear experiments were used to study subglacial sediment deformation and the development of S-matrix microstructures and microshears to constrain glacially induced deformation in diamicts. The experiments approximated subglacial conditions, and the diamict was sheared and sampled incrementally to strains of 0, 7, 18, 33, 57, and 107. At strains between 7 and 18, a steady association of S-matrix microstructures developed, which did not evolve further despite continued shearing. The IL-index, a measure of microshear-orientation strength parallel to the shearing direction correlates log-linearly with strain, which indicates its potential use as strain proxy. The ring-shear data were compared with the characteristics of Quaternary basal tills from Denmark, Poland, and Svalbard. Based On IL-index values, we conclude that these tills only experienced strain of ∼ 101, which is orders of magnitude lower than expected for deformation tills. This suggests that pervasive subglacial deformation and sediment advection in the mobile layer at the ice-bed interface may be less significant than previously assumed.

AB - Ring-shear experiments were used to study subglacial sediment deformation and the development of S-matrix microstructures and microshears to constrain glacially induced deformation in diamicts. The experiments approximated subglacial conditions, and the diamict was sheared and sampled incrementally to strains of 0, 7, 18, 33, 57, and 107. At strains between 7 and 18, a steady association of S-matrix microstructures developed, which did not evolve further despite continued shearing. The IL-index, a measure of microshear-orientation strength parallel to the shearing direction correlates log-linearly with strain, which indicates its potential use as strain proxy. The ring-shear data were compared with the characteristics of Quaternary basal tills from Denmark, Poland, and Svalbard. Based On IL-index values, we conclude that these tills only experienced strain of ∼ 101, which is orders of magnitude lower than expected for deformation tills. This suggests that pervasive subglacial deformation and sediment advection in the mobile layer at the ice-bed interface may be less significant than previously assumed.

KW - Micromorphology

KW - Strain

KW - Subglacial environment

KW - Till

U2 - 10.1130/G22629.1

DO - 10.1130/G22629.1

M3 - Journal article

AN - SCOPUS:33750086935

VL - 34

SP - 889

EP - 892

JO - Geology

JF - Geology

SN - 0091-7613

IS - 10

ER -