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紀伊半島東部, 海山地域の四万十帯上部白亜系
https://doi.org/10.14945/00000332
https://doi.org/10.14945/000003322e37ae88-5215-41ed-b498-cf5ffcffa92a
名前 / ファイル | ライセンス | アクション |
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KJ00000102378.pdf (1.4 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 紀伊半島東部, 海山地域の四万十帯上部白亜系 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | lithofacies | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | geologic structure | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | radiolarian fossils | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | illite crystallinity | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | eastern Kii | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Shimanto Belt | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Southwest Japan | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000332 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | Upper Cretaceous strata in the Shimanto Belt of the Miyama area, eastern Kii Peninsula, Southwest Japan. | |||||||
著者 |
田邊, 裕高
× 田邊, 裕高× 狩野, 謙一
WEKO
193
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書誌情報 |
静岡大学地球科学研究報告 巻 21, p. 1-10, 発行日 1994-09 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 455 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The Geology of the Shimanto Belt has been examined in the Miyama area, north of Owase, eastern Kii Peninsula, Southwest Japan. The strata in this area can be divided lithologically into three thrust-bounded formations or tectonostratigraphic units : the Mizunomitoge, Ookogawa and Shimakatsuura Formations from north to south. The Mizunomitoge Formation consists mainly of melange rocks with block-in-matrix fabrics. The Ookogawa Formation is a unit of sandstone-dominated coherent beds, and the Shimakatsuura Formation is also a unit of coherent beds mainly composed of alternating beds of sandstone and mudstone. Radiolarian fossils from these formations indicate that they are of Upper Cretaceous age. The mudstones from these formations show nearly the same illite crystallinity value belonging to the level of diagenetic and lower anchimetamorphic zones. The diagenesis and metamorphism occurred probably by the rise of geothermal gradient in a short period during the Early and Middle Miocene. The thermal maturity also suggests that these strata were accreted in a shallower tectonic level of a convergent margin. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413359 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |