{"created":"2021-03-01T06:20:41.106524+00:00","id":17624,"links":{},"metadata":{"_buckets":{"deposit":"480296be-4a7f-4e70-9b3c-c18177274d71"},"_deposit":{"id":"17624","owners":[],"pid":{"revision_id":0,"type":"depid","value":"17624"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00017624"},"item_10_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":"The Stratigraphy and Tectonic Movement in the Permian System in the S\u014dma District, Fukushima Prefecture, Japan"}]},"item_10_biblio_info_6":{"attribute_name":"\u66f8\u8a8c\u60c5\u5831","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1973-03-15","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"104","bibliographicPageStart":"91","bibliographicVolumeNumber":"7","bibliographic_titles":[{"bibliographic_title":"\u4fe1\u5dde\u5927\u5b66\u6559\u990a\u90e8\u7d00\u8981. \u7b2c\u4e8c\u90e8, \u81ea\u7136\u79d1\u5b66"}]}]},"item_10_description_20":{"attribute_name":"\u6284\u9332","attribute_value_mlt":[{"subitem_description":"In this paper the writer deals with the description of stratigraphy and geological structures, and tectonic movement during the permian period of the Soma palaeozoic deposits. The rocks of the Permian system in this area are divided into seven members by the writer (fig. 1 & 2). Uwano slate member (U\u2081), Uwano sandstone and slate member (U\u2082),\u014cashi lower conglomerate (O\u2081), \u014cashi slate and sand stone member (O\u2082), \u014cashi upper conglomrate (O\u2088), Yumiorezawa slate and sandstone member (Y\u2081), Yumiorezawa slate member (Y\u2082). The following is a simplified and precisely stratigraphy in decending order. Yumiorezawa formation: consisting of the Y\u2081 and Y\u2082 members, about 350m thick. Fossils unknown. \u014cashi formation: consisting of the O3 member in the upper part, intercalating some fossilferous limestone lenses, the O\u2082 in the middle, and the O\u2081 in the lower, about 350m thick. Important fossils: Lepidolina, Yabeina, Verbeekina, Pseudodoliolina, Parafusulina, Waagenophyllum, Wentzeloides, etc.. These fossils are restricted in their occurence to the upper and middle parts. Uwano formation: consisting of the U\u2081 and the U\u2082 members. Pseudoschwagerina was collected at two hirzones. The geological structures in the Permian system of the present deposits may be devided into two units in the deformation and destruction. The pre-Permian deposits are extensively overlain by the Uwano formation which constitutes a synclinorium with the axis of north-north-east, and the dips of 40 degree to 90. The Uwano synclinorium is overlain by the \u014cashi-Yumiorezawa basin structure consisted of two formation, both of which represent low dips of 5 degree to 30 all over the basin in sharp contrast with the general trend of the U -synclinorium, with exception of the vicinity of tectonic line and disturbed region. Judging from the sedimentary facies of the \u014cashi formation, it can be inferred that the sediments were formed in shallow water within wave action, and that the basement complex kept to rapidly sinking down during deposition of the \u014cashi formation. The \u014cashi formation is thicker in the east and south east than in the west, thining out or gradually grading into the sandstone and the slate of thin alternation of Y\u2081 member in the west side of the given deposits. The \u014cashiYumiorezawa basin structure is differ from the Dwano synclinorium, in its less complexeous geological structure. Differences between these feature are more remarkable in the east. Observation of outcrops also testified this structural feature. There is the other fact that the constituent rocks of the Oasi conglomerates consist of granitic rocks, volcanic rocks, subangular pebbles of black slate, biotite hornfels and myronitic silisious rock. Such coarse material had deposited from time to time untill the close of the Lepidolina epock in the Soma district. All that can be inferred in the Soma district are the backland situated to the east side of the present district, and uplifted abruptly after dose of the Dwano epock. This unknown backland continuousely supplied the \u014cashi formation with a large quantity of coarse material, and were from time to time worn low. They were mobile areas. Supply of such coarse sediments came to the end at the close of the L\u014c\u014cepidolina epock. Continuously the slates of the Toyoma type representing enviroment of closed sea kept on deposition during the Late Permian.","subitem_description_type":"Abstract"}]},"item_10_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_10_description_5":{"attribute_name":"\u5f15\u7528","attribute_value_mlt":[{"subitem_description":"\u4fe1\u5dde\u5927\u5b66\u6559\u990a\u90e8\u7d00\u8981. \u7b2c\u4e8c\u90e8, \u81ea\u7136\u79d1\u5b66 7: 91-104(1973)","subitem_description_type":"Other"}]},"item_10_publisher_4":{"attribute_name":"\u51fa\u7248\u8005","attribute_value_mlt":[{"subitem_publisher":"\u4fe1\u5dde\u5927\u5b66\u6559\u990a\u90e8"}]},"item_10_source_id_35":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0583-0613","subitem_source_identifier_type":"ISSN"}]},"item_10_source_id_40":{"attribute_name":"\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID","attribute_value_mlt":[{"subitem_source_identifier":"AN0012116X","subitem_source_identifier_type":"NCID"}]},"item_creator":{"attribute_name":"\u8457\u8005","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"\u4f50\u85e4,  \u654f\u5f66"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"\u30d5\u30a1\u30a4\u30eb\u60c5\u5831","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2015-09-28"}],"displaytype":"detail","filename":"Liberal_arts_S07-07.pdf","filesize":[{"value":"950.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"Liberal_arts_S07-07.pdf","url":"https://soar-ir.repo.nii.ac.jp/record/17624/files/Liberal_arts_S07-07.pdf"},"version_id":"47500816-10d9-449a-8dc4-9a62dcd82e85"}]},"item_language":{"attribute_name":"\u8a00\u8a9e","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"\u8cc7\u6e90\u30bf\u30a4\u30d7","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"\u76f8\u99ac\u53e4\u751f\u5c64(\u798f\u5cf6\u770c,\u5317\u6771\u90e8\u963f\u6b66\u9688\u5c71\u5730)\u306e\u4e8c\u7573\u7cfb\u306b\u307f\u3089\u308c\u308b\u53e4\u751f\u4ee3\u672b\u306e\u5730\u6bbb\u5909\u52d5\u306b\u3064\u3044\u3066","item_titles":{"attribute_name":"\u30bf\u30a4\u30c8\u30eb","attribute_value_mlt":[{"subitem_title":"\u76f8\u99ac\u53e4\u751f\u5c64(\u798f\u5cf6\u770c,\u5317\u6771\u90e8\u963f\u6b66\u9688\u5c71\u5730)\u306e\u4e8c\u7573\u7cfb\u306b\u307f\u3089\u308c\u308b\u53e4\u751f\u4ee3\u672b\u306e\u5730\u6bbb\u5909\u52d5\u306b\u3064\u3044\u3066"}]},"item_type_id":"10","owner":"1","path":["1702/1721/1725"],"pubdate":{"attribute_name":"\u516c\u958b\u65e5","attribute_value":"2010-02-12"},"publish_date":"2010-02-12","publish_status":"0","recid":"17624","relation_version_is_last":true,"title":["\u76f8\u99ac\u53e4\u751f\u5c64(\u798f\u5cf6\u770c,\u5317\u6771\u90e8\u963f\u6b66\u9688\u5c71\u5730)\u306e\u4e8c\u7573\u7cfb\u306b\u307f\u3089\u308c\u308b\u53e4\u751f\u4ee3\u672b\u306e\u5730\u6bbb\u5909\u52d5\u306b\u3064\u3044\u3066"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2021-03-01T09:35:59.563640+00:00"}