検索対象:     
報告書番号:
※ 半角英数字
 年 ~ 
 年

Frictional properties of Shionohira Fault Gouge, 2; A Comparison with Kuruma Fault Gouge at the southern extension of Shionohira Fault

塩ノ平断層における断層ガウジの摩擦特性,2; 車断層(塩ノ平断層南方延長部)における断層ガウジとの比較

瀬下 和芳 ; 青木 和弘 ; 田中 遊雲; 丹羽 正和   ; 嶋本 利彦*; Ma, S.*; Yao, L.*; 亀高 正男*

Seshimo, Kazuyoshi; Aoki, Kazuhiro; Tanaka, Yukumo; Niwa, Masakazu; Shimamoto, Toshihiko*; Ma, S.*; Yao, L.*; Kametaka, Masao*

The April 11, 2011 Fukushima-ken Hamadori Earthquake (the largest aftershock of the 2011 off the Pacific coast of Tohoku Earthquake) formed co-seismic surface ruptures in NNW-SSE direction in Iwaki City, Fukushima Prefecture, Japan, named Shionohira Fault (hereafter called active segment). A N-S trending geological fault with lineaments (Kuruma Fault) along the southern extension of Shionohira Fault showed no surface ruptures (hereafter called non-active segment). The current report discusses differences of active and non-active segments by conducting low to high-velocity friction experiments on the gouge from shallow borehole cores.

Access

:

- Accesses

InCites™

:

Altmetrics

:

[CLARIVATE ANALYTICS], [WEB OF SCIENCE], [HIGHLY CITED PAPER & CUP LOGO] and [HOT PAPER & FIRE LOGO] are trademarks of Clarivate Analytics, and/or its affiliated company or companies, and used herein by permission and/or license.