書誌事項
- タイトル別名
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- Mid-Holocene Underwater Jomon Sites along the West Coast of Kyushu, Japan, Hydro-isostasy and Asthenospheric Viscosity.
- Mid-Holocene Underwater Jomon Sites alo
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抄録
Mid-Holocene underwater Jomon sites typically observed along the west coast of Kyushu, Japan, are reasonably explained by the hydro-isostatic adjustment due to the last deglaciation. The distribution of these underwater Jomon sites is very sensitive to the rheological structure above 250km depth, and comparisons between observations and predictions of sea-level variations indicate a lithospheric thickness of 30-50km and an effective asthenospheric viscosity (-200km thickness) of (8-20)×1019Pa s. The viscosity contrast between the asthenosphere and the underlying upper mantle is less than 10, and a well defined low-viscosity asthenosphere may not exist even in the island arc regions such as the Japanese Islands. Thus regional postglacial sea-levels are spatio-temporally variable and dependent on crustal tilting caused by hydro-isostatic adjustment, and they might have constrained the development of prehistoric human settlements and the way of lives.
収録刊行物
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- 第四紀研究
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第四紀研究 37 (4), 315-323, 1998
日本第四紀学会
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詳細情報 詳細情報について
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- CRID
- 1390001206497072000
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- NII論文ID
- 10002510589
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- NII書誌ID
- AN0034136X
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- ISSN
- 18818129
- 04182642
- http://id.crossref.org/issn/04182642
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- NDL書誌ID
- 4590060
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可