{"_buckets": {"deposit": "ac378d13-fc18-40e8-90a6-e80334ac7a0a"}, "_deposit": {"id": "8541", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "8541"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00008541"}, "item_10_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1998-11", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "6", "bibliographicPageEnd": "753", "bibliographicPageStart": "735", "bibliographicVolumeNumber": "135", "bibliographic_titles": [{"bibliographic_title": "Geological Magazine"}]}]}, "item_10_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "Middle Triassic radiolarian bedded cherts in the Mino Belt, central Japan, include a sequence showing an abrupt facies change from the lower to the upper, where grey\u2013black bedded cherts enriched in carbonaceous matter and framboidal pyrite are overlain by brick-red hematitic bedded cherts. Brownish-yellow chert enriched in goethite and purple-red chert occur at the boundary between the grey\u2013black bedded cherts and the brick-red bedded cherts. This facies change is in accordance with stratigraphic variations of geochemical characteristics; the lower section grey\u2013black bedded cherts, compared with the upper section brick-red bedded cherts, are enriched in C_tot and S_ tot, and are characterized by lower MnO/TiO_2, higher FeO/Fe_2O_3* (total iron as Fe_2O_3) and more variable Fe_2O_3*/TiO_2 values. Some of the lower section samples, in addition, are characterized by an enrichment in some transition metals (Ni, Cu, and Zn). The covariation of mineralogical and geochemical characteristics indicates that sedimentary environments and diagenetic processes were different between the lower and the upper section bedded cherts. During the deposition of the lower section bedded cherts, the sedimentary environment was anoxic and bacterial sulphate reduction occurred during the early diagenetic stage. In contrast, the upper section bedded cherts were subjected to less reducing diagenetic processes; active sulphate reduction did not occur. The change of sedimentary environment and diagenetic process at the site of deposition is likely to be attributed to the fluctuated concentration of dissolved oxygen in the water mass of a semi-closed marginal ocean basin, which was  potentially caused by sea-level change that occurred during Middle Triassic time.", "subitem_description_type": "Abstract"}]}, "item_10_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/10289"}]}, "item_10_publisher_32": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "Cambridge University Press"}]}, "item_10_relation_11": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "http://dx.doi.org/10.1017/S0016756898001587", "subitem_relation_type_select": "DOI"}}]}, "item_10_rights_12": {"attribute_name": "\u6a29\u5229", "attribute_value_mlt": [{"subitem_rights": "Cambridge University Press"}]}, "item_10_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_10_source_id_7": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0016-7568", "subitem_source_identifier_type": "ISSN"}]}, "item_10_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "SUGITANI, KENICHIRO"}], "nameIdentifiers": [{"nameIdentifier": "23994", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "MIMURA, KOICHI"}], "nameIdentifiers": [{"nameIdentifier": "23995", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-19"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "SUGITANI_KENICHIRO_Redox_change_in_sedimentary_environments_of_Triassic_bedded_1998.pdf", "filesize": [{"value": "1.0 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1000000.0, "url": {"label": "SUGITANI_KENICHIRO_Redox_change_in_sedimentary_environments_of_Triassic_bedded_1998.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/8541/files/SUGITANI_KENICHIRO_Redox_change_in_sedimentary_environments_of_Triassic_bedded_1998.pdf"}, "version_id": "cd6f18f0-1987-4c66-a173-d45bf1e7c32c"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Redox change in sedimentary environments of Triassic bedded cherts, central Japan: possible reflection of sea-level change", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Redox change in sedimentary environments of Triassic bedded cherts, central Japan: possible reflection of sea-level change"}]}, "item_type_id": "10", "owner": "1", "path": ["312/313/314"], "permalink_uri": "http://hdl.handle.net/2237/10289", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_name_i18n": "\u516c\u958b\u65e5", "attribute_value": "2008-07-28"}, "publish_date": "2008-07-28", "publish_status": "0", "recid": "8541", "relation": {}, "relation_version_is_last": true, "title": ["Redox change in sedimentary environments of Triassic bedded cherts, central Japan: possible reflection of sea-level change"], "weko_shared_id": 3}