中央構造線活断層系(四国)の川上断層・岡村断層の再検討 : 横ずれ断層の断層線認識の新たな視点とその意義

活断層研究 Issue 17 Page 132-140 published_at 1998-12
アクセス数 : 927
ダウンロード数 : 794

今月のアクセス数 : 2
今月のダウンロード数 : 3
File
ActiveFaultResearch_17_132.pdf 573 KB 種類 : fulltext
Title ( jpn )
中央構造線活断層系(四国)の川上断層・岡村断層の再検討 : 横ずれ断層の断層線認識の新たな視点とその意義
Title ( eng )
Discovery of active fault traces based on dip-slip distribution pattern of strike-slip faults : A case study on Kawakami and Okamura faults of the Median Tectonic Line active fault system in Shikoku
Creator
Nakata Takashi
Source Title
活断層研究
Issue 17
Start Page 132
End Page 140
Abstract
We discovered active fault traces on the extension of Kawakami and Okamura faults of the Median Tectonic Line active fault system in Shikoku based on new criterion that strike-slip faults are characterized by the pattern of dip-slip distribution; the upthrown side along strike-slip faults are, in general, located on the fault blocks in the direction of relative strike-slip motion.

The northeast part of the Kawakami fault is recognized as a 13km-long NE-SW trending trace with low fault scarplets with the south side upthrown, and this does not agree with the pattern of dipslip distribution along a right-lateral strike-slip fault. Detailed interpretation of large-scale airphotographs taken by US army corps about 50 years ago, revealed ENE-WSW trending low fault scarplets across young alluvial plain, that is located on the northern extension of already mapped The scarplets are less than 1 m high up to the north.

The ENE-WSW trending Okamura fault has been only recognized as an 18km-long distinctive fault scarplet known as "Nakahagi" cliff with the south side upthrown. We examined its eastern extension and found a low ENE-WSW trending fault scarplet with the north side upthrown in the south of Niihama city. The trace continues further east about 13km with obscure fault features. We trenched the newly found fault trace at two sites and obtained geological evidence of Holocene faulting.

Thus, the geometric criterion we propose in this paper gives a quite different interpretation of fault distribution from those by the previous workers. We expect that this criterion may be tested together with the other geometric criteria on major active fault and compared with segmentation based on paleoseismological data.
Keywords
横ずれ断層
活断層詳細図
セグメンテーション
縦ずれ変位の分布パターン
中央構造線
トレンチ発掘調査
strike-slip fault
detail active fault map
segmentation
dip-slip distribution of strike-slip faulting
Median Tectonic Line
trench excavation survey
NDC
General geography. Description and travel [ 290 ]
Language
jpn
Resource Type journal article
Publisher
活断層研究会
Date of Issued 1998-12
Publish Type Version of Record
Access Rights open access
Source Identifier
[ISSN] 0918-1024
[NCID] AN10157356
[URI] http://topo.earth.chiba-u.jp/afr/index.htm