Till Fabric is a sedimentological structure characterized by the preferred orientation and arrangement of clasts within glacial till, distinguished by its formation through the deformation and deposition of sediment under glacial ice, reflecting the stress regime and flow dynamics of the glacier.
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183
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114
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2017–2026
3
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129
1–5 of 129
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183
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8
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6
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1–5 of 183
Institutions
114
Iowa State University
Ames, United States
8 h-index
16 publications
748 citations
University of Wisconsin–Madison
Madison, United States
6 h-index
9 publications
361 citations
Aarhus University
Aarhus, Denmark
5 h-index
9 publications
692 citations
University of East Anglia
Norwich, United Kingdom
4 h-index
5 publications
277 citations
Western University
London, Canada
4 h-index
9 publications
837 citations
Lehigh University
Bethlehem, United States
3 h-index
8 publications
285 citations
Wisconsin Geological and Natural History Survey
Madison, United States
3 h-index
3 publications
183 citations
Simon Fraser University
Burnaby, Canada
3 h-index
3 publications
43 citations
1–8 of 114
Venues
- Boreas
16 publications · 664 citations
14
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- Journal of Glaciology
12 publications · 676 citations
12
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- Journal of Sedimentary Research
JSR · 13 publications · 883 citations
12
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- Geological Society of America Bulletin
11 publications · 676 citations
11
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- Canadian Journal of Earth Sciences
7 publications · 373 citations
7
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