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The least square method was called the \"strain analysis technique 3\" and the average method was called the \"strain analysis technique 2\" in my paper (Hayashi, 1994). The results of both methods are fairly different. The \"c-value\" is introduced to explain the difference. The difference between the strain ellipsoid calculated using the least square method and associated strain ellipses decreases as the c-value decreases, though the difference between the strain ellipsoid calculated using the average method and associated strain ellipses does not necessarily decrease. Therefore, the strain ellipsoid obtained by the least square method is expected to approach a true strain ellipsoid as the c-value decreases, though the strain ellipsoid obtained by the average method is not expected to approach a true strain ellipsoid.", "subitem_description_type": "Other"}, {"subitem_description": "沖縄島中北部バン崎周辺の国頭層群嘉陽層の3次元歪解析を最小2乗法と平均法で行った.最小2乗法とは林(1994)の「歪解析法3」のことであり,平均法とは同じく「歪解析法2」のことである.両者の結果はかなりくい違った.これを解明するため歪楕円体の適合性をあらわすc値を導入した.最小2乗法によって得られた歪楕円体はc値が小さくなると歪楕円との差が小さくなった.しかし平均法の場合にはかならずしも小さくならない.このため,最小2乗法から得られた歪楕円体はc値が小さくなると真の歪楕円体に近づくことが期待されるが,平均法の場合には期待できない.", "subitem_description_type": "Other"}, {"subitem_description": "論文", "subitem_description_type": "Other"}]}, "item_1617186643794": {"attribute_name": "Publisher", "attribute_value_mlt": [{"subitem_1522300295150": "ja", "subitem_1522300316516": "日本情報地質学会"}]}, "item_1617186702042": {"attribute_name": "Language", "attribute_value_mlt": [{"subitem_1551255818386": "jpn"}]}, "item_1617186783814": {"attribute_name": "Identifier", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/20.500.12000/2947"}]}, "item_1617186920753": {"attribute_name": "Source Identifier", "attribute_value_mlt": [{"subitem_1522646500366": "ISSN", "subitem_1522646572813": "0388-502X"}, {"subitem_1522646500366": "NCID", "subitem_1522646572813": "AN0036643X"}]}, "item_1617186941041": {"attribute_name": "Source Title", "attribute_value_mlt": [{"subitem_1522650068558": "ja", "subitem_1522650091861": "情報地質 = Geological data processing (Geoinformatics)"}]}, "item_1617187056579": {"attribute_name": "Bibliographic Information", "attribute_value_mlt": [{"bibliographicIssueNumber": "1", "bibliographicPageEnd": "29", "bibliographicPageStart": "13", "bibliographicVolumeNumber": "6"}]}, "item_1617258105262": {"attribute_name": "Resource Type", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_1617265215918": {"attribute_name": "Version Type", "attribute_value_mlt": [{"subitem_1522305645492": "VoR", "subitem_1600292170262": "http://purl.org/coar/version/c_970fb48d4fbd8a85"}]}, "item_1617605131499": {"attribute_name": "File", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "download_preview_message": "", "file_order": 0, "filename": "Hayashi_d-02.pdf", "future_date_message": "", "is_thumbnail": false, "mimetype": "", "size": 0, "url": {"objectType": "fulltext", "url": "https://u-ryukyu.repo.nii.ac.jp/record/2002439/files/Hayashi_d-02.pdf"}, "version_id": "e22107d2-0565-43a1-8887-79297592711f"}]}, "item_title": "地質構造解析における歪楕円体の適合度c値の提唱", "item_type_id": "15", "owner": "1", "path": ["1642838338003", "1642838406414"], "permalink_uri": "http://hdl.handle.net/20.500.12000/2947", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-01-14"}, "publish_date": "2008-01-14", "publish_status": "0", "recid": "2002439", "relation": {}, "relation_version_is_last": true, "title": ["地質構造解析における歪楕円体の適合度c値の提唱"], "weko_shared_id": -1}
地質構造解析における歪楕円体の適合度c値の提唱
http://hdl.handle.net/20.500.12000/2947
http://hdl.handle.net/20.500.12000/29473dfbac67-dd7b-496b-811a-8a79851bad71
名前 / ファイル | ライセンス | アクション |
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Hayashi_d-02.pdf
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Item type | デフォルトアイテムタイプ(フル)(1) | |||||||||
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公開日 | 2008-01-14 | |||||||||
タイトル | ||||||||||
タイトル | 地質構造解析における歪楕円体の適合度c値の提唱 | |||||||||
言語 | ja | |||||||||
タイトル | ||||||||||
タイトル | Proposed Consistency c-value for Strain Ellipsoids in Geological Structure Analysis | |||||||||
言語 | en | |||||||||
作成者 |
林, 大五郎
× 林, 大五郎
× Hayashi, Daigoro
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アクセス権 | ||||||||||
アクセス権 | open access | |||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Least square method | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Average method | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Three dimensional strain analysis | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Consistency of strain | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | c-value | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 最小2乗法 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 平均法 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 3次元歪解析 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 歪の適合性 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | c値 | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | I have performed the three dimensional strain analysis of the Kayo Formation, Kunchan Group around Ban-zaki, middle north of Okinawa-jima by means of the "least square method" and "average method". The least square method was called the "strain analysis technique 3" and the average method was called the "strain analysis technique 2" in my paper (Hayashi, 1994). The results of both methods are fairly different. The "c-value" is introduced to explain the difference. The difference between the strain ellipsoid calculated using the least square method and associated strain ellipses decreases as the c-value decreases, though the difference between the strain ellipsoid calculated using the average method and associated strain ellipses does not necessarily decrease. Therefore, the strain ellipsoid obtained by the least square method is expected to approach a true strain ellipsoid as the c-value decreases, though the strain ellipsoid obtained by the average method is not expected to approach a true strain ellipsoid. | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | 沖縄島中北部バン崎周辺の国頭層群嘉陽層の3次元歪解析を最小2乗法と平均法で行った.最小2乗法とは林(1994)の「歪解析法3」のことであり,平均法とは同じく「歪解析法2」のことである.両者の結果はかなりくい違った.これを解明するため歪楕円体の適合性をあらわすc値を導入した.最小2乗法によって得られた歪楕円体はc値が小さくなると歪楕円との差が小さくなった.しかし平均法の場合にはかならずしも小さくならない.このため,最小2乗法から得られた歪楕円体はc値が小さくなると真の歪楕円体に近づくことが期待されるが,平均法の場合には期待できない. | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | 論文 | |||||||||
出版者 | ||||||||||
言語 | ja | |||||||||
出版者 | 日本情報地質学会 | |||||||||
言語 | ||||||||||
言語 | jpn | |||||||||
資源タイプ | ||||||||||
資源タイプ | journal article | |||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
出版タイプ | ||||||||||
出版タイプ | VoR | |||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
識別子 | ||||||||||
識別子 | http://hdl.handle.net/20.500.12000/2947 | |||||||||
識別子タイプ | HDL | |||||||||
収録物識別子 | ||||||||||
収録物識別子タイプ | ISSN | |||||||||
収録物識別子 | 0388-502X | |||||||||
収録物識別子 | ||||||||||
収録物識別子タイプ | NCID | |||||||||
収録物識別子 | AN0036643X | |||||||||
収録物名 | ||||||||||
言語 | ja | |||||||||
収録物名 | 情報地質 = Geological data processing (Geoinformatics) | |||||||||
書誌情報 |
巻 6, 号 1, p. 13-29 |