The effect of grain texture on the occurrence of microstructural properties in subglacial till
The effect of grain texture on the occurrence of microstructural properties in subglacial till
In this paper, we examine whether till grain size affects the range and occurrence of micromorphological features associated with subglacial shear. Our till samples were collected from two glaciers in Iceland, and varied in texture from a coarse, sandy clast-rich till (Fjallsjökull) to a fine-grained silty-sandy till (Vestari-Hagafellsjökull). We found a wide range of deformational microstructures that included skelsepic plasmic fabric, intraclasts of pre-existing eroded bedrock (basalt) and weathered clay and ‘mini-shear zones’ between clasts. We classified our micromorphological data into three classes; rotational, intermediate and linear. In addition to these observations, we performed extensive microfabric analysis at different scales on all of our samples. We found that the coarse-grained till contained a greater number and variety of microstructures than the fine-grained till. In addition, the fine-grained till showed a distinct lack of rotational structures that we attribute to the lack of significantly sized clasts in the matrix. We argue that the varied texture of the coarse-grained till provides a greater degree of perturbation within the shearing layer and so more distinct microstructures form. In a more fine-grained till, shearing is more homogeneous since there are less perturbations in the matrix and this leads to a more singular kind of microstructure. Our observations suggest that subglacial shear occurs within a multi-layered patchwork of different grain sizes, competence and pore water pressures. It is these factors that are so crucial in determining the occurrence and type of microstructural evidence we see in subglacial tills.
2501-2512
Hart, J.K.
e949a885-7b26-4544-9e15-32ba6f87e49a
Khatwa, A.
fdd97d2d-d442-4a33-ba4e-ea95abc47763
Sammonds, P.
64fe1a70-36e1-462d-bdb9-c6c9b5c012bd
2 January 2004
Hart, J.K.
e949a885-7b26-4544-9e15-32ba6f87e49a
Khatwa, A.
fdd97d2d-d442-4a33-ba4e-ea95abc47763
Sammonds, P.
64fe1a70-36e1-462d-bdb9-c6c9b5c012bd
Hart, J.K., Khatwa, A. and Sammonds, P.
(2004)
The effect of grain texture on the occurrence of microstructural properties in subglacial till.
Quaternary Science Reviews, 23 (23-24), .
(doi:10.1016/j.quascirev.2004.06.006).
Abstract
In this paper, we examine whether till grain size affects the range and occurrence of micromorphological features associated with subglacial shear. Our till samples were collected from two glaciers in Iceland, and varied in texture from a coarse, sandy clast-rich till (Fjallsjökull) to a fine-grained silty-sandy till (Vestari-Hagafellsjökull). We found a wide range of deformational microstructures that included skelsepic plasmic fabric, intraclasts of pre-existing eroded bedrock (basalt) and weathered clay and ‘mini-shear zones’ between clasts. We classified our micromorphological data into three classes; rotational, intermediate and linear. In addition to these observations, we performed extensive microfabric analysis at different scales on all of our samples. We found that the coarse-grained till contained a greater number and variety of microstructures than the fine-grained till. In addition, the fine-grained till showed a distinct lack of rotational structures that we attribute to the lack of significantly sized clasts in the matrix. We argue that the varied texture of the coarse-grained till provides a greater degree of perturbation within the shearing layer and so more distinct microstructures form. In a more fine-grained till, shearing is more homogeneous since there are less perturbations in the matrix and this leads to a more singular kind of microstructure. Our observations suggest that subglacial shear occurs within a multi-layered patchwork of different grain sizes, competence and pore water pressures. It is these factors that are so crucial in determining the occurrence and type of microstructural evidence we see in subglacial tills.
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Published date: 2 January 2004
Additional Information:
I initiated and lead this project, which is one of the first papers to report findings from an undisturbed subglacial till sample examined by thin section analysis. We show for the first time, how grain texture is a key element in understanding subglacial processes.
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Local EPrints ID: 15520
URI: http://eprints.soton.ac.uk/id/eprint/15520
ISSN: 0277-3791
PURE UUID: 26495c8f-3e58-43e6-8a7c-26a9e4fed857
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Date deposited: 20 Apr 2005
Last modified: 16 Mar 2024 02:39
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Author:
A. Khatwa
Author:
P. Sammonds
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