| Item type |
紀要論文 / Departmental Bulletin Paper(1) |
| 公開日 |
2010-11-30 |
| タイトル |
|
|
タイトル |
Some basic data on the quaternary glaciation in the chilean lake district |
| 言語 |
|
|
言語 |
eng |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
glaciation |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
piedmont glacier |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
paleosoil |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
tephra |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
Chilean Lake District |
| 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 |
Hirakawa, Kazuomi
Nogami, Michio
Imaizumi, Toshifumi
Okada, Atumasa
|
| 著者(ヨミ) |
ヒラカワ, カズオミ
ノガミ, ミチオ
イマイズミ, トシフミ
オカダ, アツマサ
|
| 抄録 |
|
|
内容記述タイプ |
Abstract |
|
内容記述 |
Significant eight figures on the Quaternary glaciation in the Chilean Lake District are presented. They are maps showing the former ice margins of four different glaciations, stratigraphies of tephras and paleosoils, and cross sections of glacial landforms. Development of coalescent piedmont glaciers during each glaciation is clearly indicated in these figures. Description on tephra-stratigraphy and red soil must be significant to examine the chronology of these glaciations. The longitudinal profiles of outwash plains along the major rivers during the Last Glaciation can be prominent evidence to discuss the chronology in relation to the lowering of the sea level. On the basis of these profiles, the largest glacier advance during the Last Glaciation probably occurred during the isotope Stage 4. |
| 書誌情報 |
Geographical Reports of Tokyo Metropolitan University
号 35,
p. 41-49,
発行日 2000
|
| 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 |
20005-35-005.pdf (354.5 kB)
