4 0 0 0 OA なぜ幼児は石を拾うのか ―香川県三木町の幼児の行動記録から―
- 著者
- 梅田 真樹 佐々木 明世
- 出版者
- 一般社団法人 日本環境教育学会
- 雑誌
- 環境教育 (ISSN:09172866)
- 巻号頁・発行日
- vol.30, no.2, pp.2_30-37, 2020 (Released:2020-12-19)
- 参考文献数
- 16
4 0 0 0 OA 保育園から始まる地学教育
- 著者
- 梅田 真樹
- 出版者
- 日本地学教育学会
- 雑誌
- みんなの地学 (ISSN:24356441)
- 巻号頁・発行日
- vol.1, pp.21, 2020-06-30 (Released:2021-12-02)
1 0 0 0 OA 飛騨外縁帯金山地域・福地地域の酸性凝灰岩層からのペルム紀中世放散虫化石
- 著者
- 梅田 真樹 江崎 洋一
- 出版者
- 日本古生物学会
- 雑誌
- 化石 (ISSN:00229202)
- 巻号頁・発行日
- vol.62, pp.37-44, 1997-06-30 (Released:2017-10-03)
- 参考文献数
- 29
The acidic tuffaceous strata in the Kanayama and Fukuji areas of the Hida "Gaien" (=Marginal) Terrane were previously designated as the Rosse Formation of Early Devonian time and the Mizuyagadani Formation of Early Permian time, respectively. However, the age of the extracted radiolarian fossils is different from the previously known age for the tuffaceous successions. The radiolarian fauna from the acidic tuffs is commonly characterized by Pseudoalbaillella fusiformis, Pseudoalbaillella sp. aff. P. longicornis and Follicucullus monacanthus, indicative of the F. monacanthus Zone of late Middle Permian. The stratigraphy should be revised thoroughly in those areas. The Middle Permian acidic tuffs are pervasive not only within the terrane but also among the adjacent terranes, indicating the prevalence of volcanic activity in the provenance. The present results are indispensable for the reconstruction of Permian paleogeography around Hida "Gaien" Terrane.
The acidic tuffaceous strata in the Kanayama and Fukuji areas of the Hida "Gaien" (=Marginal) Terrane were previously designated as the Rosse Formation of Early Devonian time and the Mizuyagadani Formation of Early Permian time, respectively. However, the age of the extracted radiolarian fossils is different from the previously known age for the tuffaceous successions. The radiolarian fauna from the acidic tuffs is commonly characterized by Pseudoalbaillella fusiformis, Pseudoalbaillella sp. aff. P. longicornis and Follicucullus monacanthus, indicative of the F. monacanthus Zone of late Middle Permian. The stratigraphy should be revised thoroughly in those areas. The Middle Permian acidic tuffs are pervasive not only within the terrane but also among the adjacent terranes, indicating the prevalence of volcanic activity in the provenance. The present results are indispensable for the reconstruction of Permian paleogeography around Hida "Gaien" Terrane.