{"_buckets": {"deposit": "55344d15-4df7-4705-87d8-0b27c27b7516"}, "_deposit": {"id": "16887", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "16887"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00016887"}, "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 Calcarious Mudstones from Tertiary Marine Sediments in the east\uff0c-side region of the Fossa Magna\uff0cCe ntral Japan\uff0ca nd its Significanc"}]}, "item_11_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1993-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "104", "bibliographicPageStart": "99", "bibliographicVolumeNumber": "15", "bibliographic_titles": [{"bibliographic_title": "\u74b0\u5883\u79d1\u5b66\u5e74\u5831"}]}]}, "item_11_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": ":A uthors found the grayish white mudstone from the fresh outcrops at the site of land development in the east-side region of the .Fossa Magna\uff0cc entral Japan. Grayish white mudstones have been observed from view points of the occurence mode and morphologicai features. Its significance has been dicussed The grayish white mudstones have been identified as calcium carabonate by chemical analysis and X-ray microanalyzer. The calcarious mudstones have been found only in the Aoki formation for the surveyable part in the region. Calcium carbonate content was the range of 4 to 83 %. The formation of calcarious mudstone was about 0.1 to 60 cm thick. The morphological features of calcarious formation were mostly alayer type\uff0ca nd occasiortally ac oncave type\uff0ca r adical type\uff0ca w edge type\uff0ca l amina type\uff0ca nd al ode type. The grayish white mudstones have been found only on the deep horizon. It was then suggested that calcarious mudstones mitigate a acidification of soil by sulfuric acid which was derived from the oxidation of pyrite by the joint action of air and rain water", "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\u583115:99-104(1993)", "subitem_description_type": "Other"}]}, "item_11_link_3": {"attribute_name": 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