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Geomorphology of the thakkhola-muktinath region, central nepal, and its late quaternary history
http://hdl.handle.net/10748/3524
http://hdl.handle.net/10748/35241850220e-00f6-4691-832b-099d4c26de85
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
20005-19-005.pdf (1.9 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
|---|---|---|---|---|---|---|---|---|
| 公開日 | 2010-11-30 | |||||||
| タイトル | ||||||||
| タイトル | Geomorphology of the thakkhola-muktinath region, central nepal, and its late quaternary history | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| 資源タイプ | ||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
| 資源タイプ | departmental bulletin paper | |||||||
| 著者 |
Iwata, Shuji
× Iwata, Shuji
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| 著者(ヨミ) |
イワタ, シュウジ
× イワタ, シュウジ |
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| 抄録 | ||||||||
| 内容記述タイプ | Abstract | |||||||
| 内容記述 | Glacial and mass-movement landforms, river terraces, and the sediments forming these landforms were surveyed in the field, and the origin, relative chronology and crustal movement were discussed in the upper basin of the Kali Gandaki River. Large scale land-slides and glacial deposits around Larjung played an important role for making up the geomorphology of the Thakkhola basin: These landslides made a distinct basin-form and the glacier deposits dammed up the Kali Gandaki and then formed the Paleo Marpha Lake, in which the Marpha Formation accumulated. These occurred in the Pre-Last Interglacial period. The Marpha Formation was entrenched and filled with fluvioglacial materials in the Early and Late Substages of the Last Glacial. | |||||||
| 書誌情報 |
Geographical Reports of Tokyo Metropolitan University 号 19, p. 25-42, 発行日 1984 |
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| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 03868710 | |||||||
| 書誌レコードID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA00200173 | |||||||
| 著者版フラグ | ||||||||
| 出版タイプ | VoR | |||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||
| 出版者 | ||||||||
| 出版者 | Department of Geography, Tokyo Metropolitan University | |||||||
