{"_buckets": {"deposit": "02a936cf-28f6-414c-9e2f-63e5b524ac51"}, "_deposit": {"id": "32803", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32803"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032803", "sets": []}, "author_link": ["127693", "127694", "127695", "127690", "127691", "127692"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u5730\u96fb\u4f4d\u5dee\u540c\u6642\u9023\u7d9a\u89b3\u6e2c\u306b\u3088\u308b\u5730\u9707\u4e88\u77e5\u7814\u7a76\u5831\u544aI : \u89b3\u6e2c\u7db2\u306e\u8a2d\u7f6e"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1989-09-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "311", "bibliographicPageStart": "255", "bibliographicVolumeNumber": "64", "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": "In order to test the applicability of the VAN-method of short term earthquake prediction which has reportedly been extremely successful in Greece, a telluric potential monitoring network has been set up in Japan under a cooperative program with the Nippon Telegraph an Telephone Corporation (NTT). So far, 22 stations have been tested. Mainly due to logistic and financial constrainst, at all except two temporary stations existing NTT electrodes are used. At each station, telluric potential difference is sampled every 20 seconds on six dipoles set in different lengths and azimuths. Data stored at each station are transmitted to the central station at the Earthquake Research Institute (ERI) by telephone once a day. At several stations artificial noise is too high even to detect the potential changes due to geomagnetic variations but there are some stations yielding reasonably noise-free data.", "subitem_description_type": "Abstract"}, {"subitem_description": 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