Late Quaternary activity of the Iida-Matsukawa fault in the southern Ina valley, Japan.
Bibliographic Information
- Other Title
-
- 伊那谷南部の飯田‐松川断層の第四紀後期の活動性
- イナダニ ナンブ ノ イイダ マツカワ ダンソウ ノ ダイ4キ コウキ ノ カツドウセイ
Search this article
Abstract
Geological and topographical investigations show that the Iida-Matsukawa fault striking northwest and extending for about 15 km in the southern Kiso Range, central Japan, is presently active with a horizontal slip rate of 1 mm/y. It is inferred that the Kiso Range is displaced about 2 km sinistrally and 500 m vertically. Many valleys were systematically sinistrally-deflected or bent at the fault trace. There is a linear relation of D=aL between the offset(D) and the length (L) of upper valley channel from the deflected point, where coefficient a is limited in a range of 0.08∼0.3. Detailed field observations show that the terrace containing AT volcanic ash formed 20, 000 y.B.P is displaced 3∼5 m vertically. The analysis of foliated cataclastic rocks shows that the fault formed before the Quaternary and moved as a sinistral strike-slip fault with a normal displacement component since it formed.
Journal
-
- The Journal of the Geological Society of Japan
-
The Journal of the Geological Society of Japan 106 (6), 413-425, 2000
The Geological Society of Japan
- Tweet
Keywords
Details 詳細情報について
-
- CRID
- 1390282681212272512
-
- NII Article ID
- 110003013122
- 10008433681
-
- NII Book ID
- AN00141768
-
- COI
- 1:CAS:528:DC%2BD3cXksFOktLo%3D
-
- ISSN
- 13499963
- 00167630
-
- NDL BIB ID
- 5439126
-
- Text Lang
- ja
-
- Data Source
-
- JaLC
- NDL
- Crossref
- CiNii Articles
-
- Abstract License Flag
- Disallowed