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The Aomori Bay West Coast Fault Zone (青森湾西岸断層帯, Aomoriwan-seigan Dansō-tai) is an active fault zone on the Tsugaru Peninsula in Aomori Prefecture and its capital city, Aomori. It is paralleled to east by the west coast of Aomori Bay and to the west by the Tsugaru Mountains, running from north-northwest to south-southeast on the peninsula, through the city of Aomori, and finally extending south toward the Hakkōda Mountains. The zone is made up of three faults: the Aomori Bay West Fault, the Nogiwa Fault, and the Nyunai Fault. The Nyunai fault is a reverse fault.

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dbo:abstract
  • The Aomori Bay West Coast Fault Zone (青森湾西岸断層帯, Aomoriwan-seigan Dansō-tai) is an active fault zone on the Tsugaru Peninsula in Aomori Prefecture and its capital city, Aomori. It is paralleled to east by the west coast of Aomori Bay and to the west by the Tsugaru Mountains, running from north-northwest to south-southeast on the peninsula, through the city of Aomori, and finally extending south toward the Hakkōda Mountains. The zone is made up of three faults: the Aomori Bay West Fault, the Nogiwa Fault, and the Nyunai Fault. The Nyunai fault is a reverse fault. (en)
  • 아오모리만 서안 단층대(일본어: 青森湾西岸断層帯 あおもりわんせいがんだんそうたい[*])는 일본 아오모리현에 있는 단층대이다. 서부 아오모리만 단층(Aomoriwan West Fault), 노기와 단층(Nogiwa Fault), 뉴나이 단층(Nyunai Fault)으로 구성된다. 요모기타촌(蓬田村)에서 히가시쓰가루군(青森県東津軽郡)을 거쳐 아오모리시까지 연장된다. 대체로 남-북 주향에 31km정도의 연장을 가지는 역단층이다. (ko)
  • 青森湾西岸断層帯(あおもりわんせいがんだんそうたい)は、青森湾南西岸から青森市西方にかけて分布する活断層帯である。 (ja)
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dbp:age
  • Miocene-recent (en)
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dbp:displacement
  • 3.15576E10
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  • Aomori Prefecture with the Aomori Bay West Coast Fault Zone shown in red (en)
dbp:name
  • Aomori Bay West Coast Fault Zone (en)
dbp:orogeny
  • North Kitakami Belt (en)
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  • Aomoriwan-seigan Dansō-tai (en)
  • 青森湾西岸断層帯 (en)
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  • Japan Tohoku (en)
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  • Location in Tohoku (en)
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  • Aomori Bay West Fault, Nogiwa Fault, Nyunai Fault (en)
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rdfs:comment
  • The Aomori Bay West Coast Fault Zone (青森湾西岸断層帯, Aomoriwan-seigan Dansō-tai) is an active fault zone on the Tsugaru Peninsula in Aomori Prefecture and its capital city, Aomori. It is paralleled to east by the west coast of Aomori Bay and to the west by the Tsugaru Mountains, running from north-northwest to south-southeast on the peninsula, through the city of Aomori, and finally extending south toward the Hakkōda Mountains. The zone is made up of three faults: the Aomori Bay West Fault, the Nogiwa Fault, and the Nyunai Fault. The Nyunai fault is a reverse fault. (en)
  • 아오모리만 서안 단층대(일본어: 青森湾西岸断層帯 あおもりわんせいがんだんそうたい[*])는 일본 아오모리현에 있는 단층대이다. 서부 아오모리만 단층(Aomoriwan West Fault), 노기와 단층(Nogiwa Fault), 뉴나이 단층(Nyunai Fault)으로 구성된다. 요모기타촌(蓬田村)에서 히가시쓰가루군(青森県東津軽郡)을 거쳐 아오모리시까지 연장된다. 대체로 남-북 주향에 31km정도의 연장을 가지는 역단층이다. (ko)
  • 青森湾西岸断層帯(あおもりわんせいがんだんそうたい)は、青森湾南西岸から青森市西方にかけて分布する活断層帯である。 (ja)
rdfs:label
  • Aomori Bay West Coast Fault Zone (en)
  • 아오모리만 서안 단층대 (ko)
  • 青森湾西岸断層帯 (ja)
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