{"_buckets": {"deposit": "aabd96c1-17e9-4d04-9609-038d39aab893"}, "_deposit": {"id": "32839", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32839"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032839", "sets": []}, "author_link": ["127955", "127956", "127957", "127958", "127959", "127960", "127961", "127948", "127949", "127950", "127951", "127952", "127953", "127954"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Leveling Survey across the Zenkoji Earthquake Fault in the City of Nagano"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1988-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "515", "bibliographicPageStart": "501", "bibliographicVolumeNumber": "62", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "\u9577\u91ce\u5e02\u8857\u5730\u3092\u8d70\u308b\u5584\u5149\u5bfa\u5730\u9707\u65ad\u5c64\u3092\u6a2a\u65ad\u3059\u308b4\u672c\u306e\u8def\u7dda\u304b\u3089\u306a\u308b46\u70b9\u306e\u7a20\u5bc6\u306a\u6c34\u6e96\u7db2\u3092\u5f35\u308a,1986\u5e743\u6708\u30681987\u5e743\u6708\u306e2\u56de,\u7cbe\u5bc6\u6c34\u6e96\u6e2c\u91cf\u3092\u5b9f\u65bd\u3057\u305f.\u5f80\u5fa9\u5dee\u306e\u7d71\u8a08\u304b\u3089,\u6c34\u6e96\u70b9\u306e\u5404\u533a\u9593\u306e\u6c34\u6e96\u5909\u52d5\u306e\u5076\u7136\u8aa4\u5dee(\u6a19\u6e96\u504f\u5dee)\u306f0.3mm\u3067\u3042\u308b.3\u3064\u306e\u74b0\u306e\u9589\u5408\u5dee\u304b\u3089\u6c42\u3081\u305f\u7d2f\u7a4d\u8aa4\u5dee\u306f,1\u70b9\u5f53\u308a0.1mm\u4ee5\u4e0b\u3067\u3042\u3063\u305f.1\u5e74\u9593\u306e\u6c34\u6e29\u5909\u52d5\u306f\u6c34\u6e96\u7db2\u5168\u4f53\u306b\u5bfe\u3057\u3066,\u5317\u4e0b\u308a\u5357\u4e0a\u308a\u306e\u50be\u52d5\u3092\u793a\u3059.\u305d\u306e\u5927\u304d\u3055\u306f,2.5\uff5e2.6\u00d710-6rad/year\u3067\u3042\u3063\u3066,\u677e\u4ee3\u7fa4\u767a\u5730\u9707\u76f4\u5f8c\u306e\u3053\u306e\u5730\u57df\u306e\u50be\u5411\u3068\u306f\u9006\u306e\u30bb\u30f3\u30b9\u3067\u3042\u308b.\u6c34\u6e96\u70b9\u8fd1\u508d\u306e\u74b0\u5883\u3084\u76f4\u4e0b\u306e\u5730\u76e4\u306e\u5f71\u97ff\u3068\u601d\u308f\u308c\u308b\u5c40\u6240\u7684\u306a\u7570\u5e38\u3092\u9664\u3051\u3070,\u65ad\u5c64\u3092\u5883\u3068\u3057\u305f\u660e\u77ad\u306a\u897f\u4e0a\u308a\u6771\u843d\u3061\u306e\u5909\u52d5\u306f\u898b\u3044\u51fa\u305b\u306a\u304b\u3063\u305f.", "subitem_description_type": "Abstract"}, {"subitem_description": "Precise leveling has been conducted across the Zenkoji Earthquake Fault in the central part of the city of Nagano in central Honshu, Japan. The bench marks, totaling 46, form four routes across the fault and three circuits. The first leveling was carried out in March, 1986 and the second in March, 1987. The standard deviation of accidental errors for the changes of relative heights is estimated to be 0.3 mm, with cummulative errors within 0.1 mm for each point. One year period leveling change shows tilting movement dipping to the north, with the slope of (2.5-2.6)\u00d71O-6 rad/year. This region had once been in the field of tilt dipping nearly south in 1969-1977. The recent trend revealed by the leveling survey is nearly opposite. Any significant level changes across the fault cannot be recognized except for one route, where the eastern side of the fault has subsided up to 1.4 mm in comparison with the opposite side. Even along this route, the vertical displacement of 2-3 cm, with the eastern down, discovered on the pavement in front of the entrance of the prefectural office, just near the fault, cannot be attributed to crustal movement, because the level change was less than 0.4 mm per year for the span of 100 m across the fault, which would have yielded an offset of eight milimeters at most during the past 20 years.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "127955", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Tsukuda, Tameshige"}]}, {"nameIdentifiers": [{"nameIdentifier": "127956", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Izutuya, Sadakatsu"}]}, {"nameIdentifiers": [{"nameIdentifier": "127957", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Haneda, Toshio"}]}, {"nameIdentifiers": [{"nameIdentifier": "127958", "nameIdentifierScheme": 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