{"_buckets": {"deposit": "f4c145c5-18df-4aed-a414-92c58f0c2bc9"}, "_deposit": {"id": "11868", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11868"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00011868", "sets": ["1169:1170"]}, "author_link": ["36346", "36347", "36348", "36349", "36350", "36351", "36352"], "control_number": "11868", "item_1628147817048": {"attribute_name": "\u51fa\u7248\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_6_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1978", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "suppl", "bibliographicPageEnd": "366", "bibliographicPageStart": "357", "bibliographicVolumeNumber": "26", "bibliographic_titles": [{"bibliographic_title": "Journal of Physics of the Earth"}]}]}, "item_6_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The late Mesozoic to early Neogene geosyncline in the Outer zone of Southwest Japan has been studied in detail in the Kii Peninsula by the Research Group for the Shimanto Geosyncline. The existence of the Kuroshio Paleoland to the south of the geosyncline was inferred by various sedimentologic evidences. The Shimanto belt in the Kii Peninsula is divided from north to south into three zones of Cretaceous, Eocene and Oligocene to lower Miocene. In these belts thick geosynclinal sediments were accumulated showing coarsening upward. The southward migration of the basin occurred in Cretaceous/Eocene, Eocene/Oligocene, and in early Miocene. In the present paper the reconstruction of paleogeography of the Shimanto geosyncline was attempted and the Kuroshio Paleoland was discussed in relation to the geohistory of the Philippine Sea. In spite of the detailed geologic survey in the Kii Peninsula there is no evidence of large exotic blocks nor tectonic m\u00e9langes, and this does not support the plate tectonic model ofthe Pacific-type orogeny for the Shimanto belt.", "subitem_description_type": "Abstract"}]}, "item_6_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_6_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_6_description_5": {"attribute_name": "\u5f15\u7528", "attribute_value_mlt": [{"subitem_description": "Journal of Physics of the Earth. 26(suppl):357-366 (1978)", "subitem_description_type": "Other"}]}, "item_6_link_3": {"attribute_name": 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