(PDF) Newly Found Kentoyama Fault in the Northern Part of

Newly Found Kentoyama Fault in the Northern Part of the Eastern Marginal Area of Fukui Plain, and Its Implications.

The Quaternary Research (Daiyonki-Kenkyu)

doi 10.4116/jaqua.40.67

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Date

January 1, 2001

Authors

Daisuke Hirouchi

Ken-ichi Yasue

Publisher

Japan Association for Quaternary Research

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Amanote Research

Newly Found Kentoyama Fault in the Northern Part of the Eastern Marginal Area of Fukui Plain, and Its Implications.

The Quaternary Research (Daiyonki-Kenkyu)

doi 10.4116/jaqua.40.67

Full Text

Abstract

Date

Authors

Publisher

Related search

Investigation of the Fukui-Earthquake Fault in the Fukui Plain by Means of Array Observation of Microtremors

Underground Structure in the Fukui Plain

Subsurface Geology in the Eastern Part of the Nohbi Plain, Aichi Prefecture, Central Japan

Extracellular Enzyme Activity and Its Implications for Organic Matter Cycling in Northern Chinese Marginal Seas

Rupture History of the Sakaitoge Fault During the Holocene in the Northern Part of the Sakaitoge-Kamiya Fault Zone, Central Japan

Assessment of Groundwater Pollution and Its Causes in the Plain Area of Yili River Valley

Constraints on Rock Uplift in the Eastern Transverse Ranges and Northern Peninsular Ranges and Implications for Kinematics of the San Andreas Fault in the Coachella Valley, California, USA

Northern and Middle Chichibu Belts of the Eastern Part of the Kanto Mountains, Central Japan.

S-Wave Seismic Reflection Profiling in the Northern Area of the Omiya Upland: Uplift Rate During Late Quaternary Raised by the Ayasegawa Fault in the Kanto-Heiya-Hokuseien (Northwestern Margin of the Kanto Plain) Fault Zone, Central Japan