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Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Science / Faculty of Science >
Peer-reviewed Journal Articles, etc >
北海道シューパロ川流域に分布する白亜系の地質と浮遊性有孔虫化石層序
| Title: | 北海道シューパロ川流域に分布する白亜系の地質と浮遊性有孔虫化石層序 |
| Other Titles: | Geology and planktonic foraminiferal biostratigraphy of Cretaceous strata distributed along the Shuparo River,Hokkaido,Japan |
| Authors: | 高嶋, 礼詩1 Browse this author | | 西, 弘嗣2 Browse this author | | 斎藤, 常正3 Browse this author | | 長谷川, 卓4 Browse this author |
| Authors(alt): | Takashima, Reishi1 | | Nishi, Hiroshi2 | | Saito, Tsunemasa3 | | Hasegawa, Takashi4 |
| Keywords: | Hokkaido | | Yezo Group | | Early Cretaceous | | planktonic foraminifera | | biostratigraphy | | olistostrome | | "Orbitolina-Praecaprotina limestone" |
| Issue Date: | 15-Jun-1997 |
| Publisher: | 日本地質学会 |
| Journal Title: | 地質學雜誌 |
| Journal Title(alt): | Journal of the Geological Society of Japan |
| Volume: | 103 |
| Issue: | 6 |
| Start Page: | 543 |
| End Page: | 564 |
| Abstract: | A continuous sequence of the lower and middle parts of the Cretaceous Yezo Group is exposed in the northern part of the Oyubari area, central Hokkaido. This group, striking in a north-south direction, consists chiefly of turbidite and interbedded hemipelagic mudstone sequences and intercalates a prominent olistostrome unite in its lower part.
The lower and middle parts of Yezo Group in the studied area comprise the following five formations in ascending order: the Tomitoi Formation (sandstone-dominants alternative beds of sandstone and mudstone), the Shuparogawa Formation (thinly alternating beds of sandstone and mudstone, including Orbitolina-Praecaprotina limestone olistolith in its middle part), the Maruyama Formation (debris flow deposits and tuffaceous sandstone), the Hikagenosawa Formation (laminated mudstone and massive mudstone), and the Takinosawa Formation (mudstone-dominant alternating beds of mudstone and sandstone).
These formations yield the following planktonic foraminiferal species which are useful for interregional correlation: Globigerinelloides duboisi, Hedbergella gorbachilae, Ticinella primula, Biticinella breggiensis, Rotalipora subticinesis, Rotalipira brotzeni, Rotalipora cushmani, and Helvetoglo-botruncana Helvetica. Based on the stratigraphic distribution of these age-diagnostic species, the Tomitoi Formation and the middle part of the Shuparogawa Formation are correlated with the late Aptian Stage, the upper part of the Shuparogawa Formation and the lower part of the Hikagenosawa Formation with the Albian Stage, the middle part of the Hikagenosawa Formation and the lowermost part of the Takinosawa Formation with the Cenomanian Stage, and the lower part of the Takinosawa Formation with the Turonian Stage. |
| Type: | article |
| URI: | http://hdl.handle.net/2115/17247 |
| Appears in Collections: | 理学院・理学研究院 (Graduate School of Science / Faculty of Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)
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Submitter: 高嶋 礼詩
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