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http://dbpedia.org/resource/Aomori_Bay_West_Coast_Fault_Zone
http://dbpedia.org/ontology/abstract The Aomori Bay West Coast Fault Zone (青森湾西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.ault. The Nyunai fault is a reverse fault. , 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。 , 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.
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http://dbpedia.org/property/age Miocene-recent
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http://dbpedia.org/property/displacement 3.15576E10
http://dbpedia.org/property/imageCaption Aomori Prefecture with the Aomori Bay West Coast Fault Zone shown in red
http://dbpedia.org/property/name Aomori Bay West Coast Fault Zone
http://dbpedia.org/property/orogeny North Kitakami Belt
http://dbpedia.org/property/otherName Aomoriwan-seigan Dansō-tai , 青森湾西岸断層帯
http://dbpedia.org/property/plate Okhotsk
http://dbpedia.org/property/pushpinMap Japan Tohoku
http://dbpedia.org/property/pushpinMapCaption Location in Tohoku
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http://dbpedia.org/property/region http://dbpedia.org/resource/T%C5%8Dhoku_region +
http://dbpedia.org/property/segments Aomori Bay West Fault, Nogiwa Fault, Nyunai Fault
http://dbpedia.org/property/status http://dbpedia.org/resource/Active_fault +
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rdfs:comment The Aomori Bay West Coast Fault Zone (青森湾西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.ault. The Nyunai fault is a reverse fault. , 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. , 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。
rdfs:label Aomori Bay West Coast Fault Zone , 青森湾西岸断層帯 , 아오모리만 서안 단층대
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