書誌事項
- タイトル別名
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- Subglacial Deforming Bed in the Tottabetsu Valley, the Hidaka Mountain Range
- ヒダカ サンミャク トッタベツダニ ニ オケル ヒョウガテイ ヘンケイ チソウ ニ ツイテ
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In recent years, the “subglacial deforming bed” has attracted attention as a factor of glacier dynamics. Subglacial deforming beds, named T8-till and T9-till respectively in this study, were formed at two locations in the Hidak Mountain Range during the glacier's maximum advance (Poroshiri Stade) of the Last Glacial Stage. These subglacial deforming beds are characterized by deformation structures such as shear planes, folds and fault gouge formed under compaction in the vertical direction and drag in the horizontal direction. T8-till and T9-till had been deformed by two cycles and one cycle of glacial advance and retreat, respectively. Strain at these subglacial deforming beds reconstructed using shear angle and degree of fracturing indicate that T8-till developed beneath the first warm-based and the second coldbased glaciers, while T9-till was beneath the cold-based glacier.
収録刊行物
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- 地学雑誌
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地学雑誌 111 (4), 519-530, 2002
公益社団法人 東京地学協会
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詳細情報 詳細情報について
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- CRID
- 1390001204230787840
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- NII論文ID
- 10009482989
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- NII書誌ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL書誌ID
- 6277331
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- データソース種別
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- JaLC
- NDL
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