{"_buckets": {"deposit": "41dc9011-8629-40ed-9b0b-d9b2dfa27abb"}, "_deposit": {"id": "16988", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "16988"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00016988", "sets": []}, "author_link": ["48568", "48569", "48570"], "item_11_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\uff08\u5225\u8a00\u8a9e\u7b49\uff09\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "On the Microscopic Pyrites in the N eogene Marine Sediments in Ueda region\uff0cNagano Prefecture\uff0cCe ntral Japan"}]}, "item_11_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1989-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "42", "bibliographicPageStart": "33", "bibliographicVolumeNumber": "11", "bibliographic_titles": [{"bibliographic_title": "\u74b0\u5883\u79d1\u5b66\u5e74\u5831"}]}]}, "item_11_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The microscopic pyrite occures in the bluish gray mudstones\uff0cb luish gray sandstones or the black shales. Scanning electron microscope observations have shown that there are various forms of pyrites in Ogawa-\uff0cBessho-\uff0cAoki-\uff0ca nd Uchimura formation in Ueda region. The pyrites were made up of spherical aggregates of microcrystals termed framboid and the single euhedral crystal containing mainly hexahedron\uff0coctaherdron and pentagonal dodecahedron. The framboidal pyrites were composed of various shapes of single crystals. The crystal habits of microcrystals forming the framboids were octahedron\uff0ch exoctahedron and pentagonal dodecahedron. The framboids have various diameters ranging from 2t o 100um\uff0cho wever\uff0cthese are concentrated at the lower end of this range. The diameters of the microcrystals contained in the framboids were in various sizes from 0.3 to 5um. The sections of framboid constructed from pentagonal dodecahedral crystals showed ar egular honeycomb-likepattern of hexagons. The single euhedral crystals\uff0con the other hand\uff0cwere in various sizes from 0.5 to 270um. The occurrence of microscopic pyrite must be a sign of strong reduction of the sediment at the early stage of sedimentation-diagenesis of mudstone\uff0csa ndstone and shale in the Ueda region", "subitem_description_type": "Abstract"}]}, "item_11_description_30": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7\uff08\u30b3\u30f3\u30c6\u30f3\u30c4\u306e\u7a2e\u985e\uff09", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_11_description_31": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8\uff1amime\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_11_description_5": {"attribute_name": "\u5f15\u7528", "attribute_value_mlt": [{"subitem_description": "\u74b0\u5883\u79d1\u5b66\u5e74\u583111:33-42(1989)", "subitem_description_type": "Other"}]}, "item_11_link_3": {"attribute_name": 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