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"\u6771\u4eac\u5e1d\u570b\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University"}]}]}, "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": "It was already reported by the writer in No. 6 of this Bulletin that, 1) The distribution of the foci of aftershocks of the Tango earthquake was extremely dense towards the west of the Gomura fault and also towards the south of the Yamada fault, whilst in the east of the former fault it was very rare.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "135069", "nameIdentifierScheme": "WEKO"}], "names": 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