前へ個別火山体一覧次へ

271
449古期御嶽火山別名 日本の火山第1版  55 
火山番号70 日本の火山第2版  70 
火山名御嶽 活火山カタログ  37 
個別火山体の位置 火山体番号  70-8 

 著 者 小林武彦 (改 林 信太郎)

位置と大きさ
      地形的  主火道 
 緯  度    35゜53′23″ 
 経  度    137゜29′01″ 
 最高点高度  2296 m
 基盤高度  1800 m
 分布面積   km2
 火山体体積  41  km3

活動時代と性質
 噴出物の分類  溶岩,降下火砕物層,火砕流堆積物 
 火山体の分類  SC 
 層序  0.75 - 0.42 Ma [4] 0.78 - 0.39 Ma [5]  
 年代測定値  K-Ar (peak comparison, groundmass) Western area, Kuragoehara Lava, 0.53 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.53 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.55 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.5 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.5 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.52 ± 0.02 Ma [4] Western area, Kuragoehara Lava, 0.53 ± 0.02 Ma [4] Western area, Makuiwagawa Lava, 0.61 ± 0.02 Ma [4] Western area, Hakotani Lava, 0.64 ± 0.02 Ma [4] Western area, Shiranunodani Lava, 0.63 ± 0.02 Ma [4] Western area, Shiranunodani Lava, 0.65 ± 0.02 Ma [4] Western area, Shiranunodani Lava, 0.66 ± 0.02 Ma [4] Western area, Tsuchiurazawa Lava, 0.65 ± 0.03 Ma [4] Southeastern area, Mikasayama Lava, 0.43 ± 0.02 Ma [4] Southeastern area, Mikasayama Lava, 0.44 ± 0.02 Ma [4] Southeastern area, Mikasayama Lava, 0.42 ± 0.01 Ma [4] Southeastern area, Mizuguchigawa Lava, 0.6 ± 0.03 Ma [4] Southeastern area, Suzugasawa Lava, 0.65 ± 0.03 Ma [4] Southeastern area, Kuragoehara Lava, 0.74 ± 0.02 Ma [4] Southeastern area, Kuragoehara Lava, 0.74 ± 0.02 Ma [4] Southeastern area, Kuragoehara Lava, 0.73 ± 0.02 Ma [4] Southeastern area, Kuragoehara Lava, 0.73 ± 0.03 Ma [4] Eastern area, Kuragoehara Lava, 0.67 ± 0.02 Ma [4] Eastern area, Makuiwagawa Lava, 0.69 ± 0.02 Ma [4] Eastern area, Makuiwagawa Lava, 0.71 ± 0.02 Ma [4] Eastern area, Tsuchiurazawa Lava, 0.72 ± 0.03 Ma [4] Northern area, Nunokawa Lava, 0.63 ± 0.02 Ma [4] Northern area, Nunokawa Lava, 0.72 ± 0.03 Ma [4] Northern area, Nunokawa Lava, 0.72 ± 0.02 Ma [4] Northern area, Sengendaru Lava, 0.081 ± 0.023 Ma [4] Northern area, Kuragoehara Lava, 0.68 ± 0.02 Ma [4] Northern area, Kuragoehara Lava, 0.7 ± 0.03 Ma [4] Northern area, Kuragoehara Lava, 0.69 ± 0.02 Ma [4] Northern area, Makuiwagawa Lava, 0.7 ± 0.03 Ma [4] Northern area, Tsuchiurazawa Lava0.71 ± 0.02 Ma [4] K-Ar (isotope dilution, groundmass) West, Sw, 0.464 ± 0.007 Ma [5] West, Oc, 0.504 ± 0.007 Ma [5] West, Mu, 0.597 ± 0.009 Ma [5] West, Hn, 0.645 ± 0.01 Ma [5] West, Km7, 0.66 ± 0.01 Ma [5] West, Km6, 0.678 ± 0.011 Ma [5] West, Km5, 0.67 ± 0.01 Ma [5] West, Km4, 0.681 ± 0.01 Ma [5] West, Km3, 0.662 ± 0.015 Ma [5] West, Km2, 0.707 ± 0.012 Ma [5] West, Km1, 0.693 ± 0.021 Ma [5] West, Hy, 0.699 ± 0.01 Ma [5] Southwest, Kka, 0.5 ± 0.007 Ma [5] Southwest, Ht, 0.588 ± 0.008 Ma [5] Southwest, Kda, 0.605 ± 0.009 Ma [5] Southwest, Ho, 0.594 ± 0.009 Ma [5] South, On, 0.438 ± 0.006 Ma [5] South, Kkb, 0.502 ± 0.007 Ma [5] South, Kt, 0.526 ± 0.008 Ma [5] South, Kdb, 0.586 ± 0.018 Ma [5] South, Wg, 0.618 ± 0.009 Ma [5] South, Sk, 0.711 ± 0.012 Ma [5] Southeast, Mk, 0.393 ± 0.006 Ma [5] Southeast, Mz, 0.503 ± 0.007 Ma [5] Southeast, Ok, 0.635 ± 0.01 Ma [5] Southeast, Ot, 0.662 ± 0.01 Ma [5] Southeast, Kg2, 0.694 ± 0.01 Ma [5] Southeast, Kg1, 0.697 ± 0.01 Ma [5] East, Mm, 0.615 ± 0.009 Ma [5] East, St, 0.619 ± 0.009 Ma [5] East, Ut, 0.577 ± 0.028 Ma [5] East, Ut(S), 0.597 ± 0.088 Ma [5] East, Td, 0.709 ± 0.011 Ma [5] East, Nt, 0.724 ± 0.014 Ma [5] East, Fm, 0.774 ± 0.014 Ma [5] East, Mt, 0.732 ± 0.016 Ma [5] East, Iz, 0.612 ± 0.047 Ma [5] East, Iz(S), 0.779 ± 0.136 Ma [5] East, Kr, 0.642 ± 0.01 Ma [5] East, Mh, 0.635 ± 0.01 Ma [5] East, Yua, 0.695 ± 0.01 Ma [5] East, Yub, 0.695 ± 0.01 Ma [5] North, Tna, 0.978 ± 0.01 Ma [5] North, Tnb, 0.661 ± 0.01 Ma [5] North, Oba, 0.679 ± 0.01 Ma [5] North, Obb, 0.687 ± 0.01 Ma [5] North, Sg2, 0.676 ± 0.011 Ma [5] North, Sg1, 0.695 ± 0.01 Ma [5] North, Ku, 0.711 ± 0.01 Ma [5]  

岩石名
 玄武岩  あり 
 玄武岩質安山岩  主要 
 安山岩  多い 
 デイサイト  あり 
 流紋岩  なし 
 その他   

 化学分析値 
 Aug-ol basalt (SiO2=50.8 %); Hyp+-bg. ol-aug basaltic andesite (SiO2=50.3-52.4 %); Aug-bg. ol basaltic andesite (SiO2=51.1 %); Aphyric basaltic andesite (SiO2=53.2%); Hyp-aug andesite (SiO2=54.1 %); Ol-bg. aug-hyp andesite (SiO2=55.2 %); Aug-hyp andesite (SiO2=56.9-62.8 %); Aug-hyp-ho andesite (SiO2=59.9-61.4 %); Ho-bg. ol-aug-hyp andesite (SiO2=59.1-63.9 %); Aug+-bg. ho-hyp dacite (SiO2=65.4-67.3 %) [1]  

引用文献
1 山田直利・小林武彦(1988)「御嶽山地域の地質」、地域地質研究報告(5万分の1地質図幅)、地質調査所、136p.  Yamada, N. and Kobayashi, T. (1988) Geology of Ontakesan district. With Geological Sheet Map at 1:50,000, Geol.Surv.Japan, 136p. 1103
2  Matsumoto, A. and Kobayashi, T. (1995) K-Ar determination of late Quaternary volcanic rocks using the "mass fractionation correction procedure": application to the Younger Ontake Volcano, central Japan. Chemical Geology (Isotope Geoscience Section), vol. 125, p. 123-135. 46
3 小林武彦(1993)御嶽火山の活動史と噴出物の体積計測.文部省科学研究費「火山災害の規模と特性」報告書,p.87-96. Kobayashi, T. (1993) Production rate and K-Ar datings of Ontake volcano. Report for Grant of the Japanese ministry of Education, Science and culture "The volume and characteristics of volcanic disasters", p. 87-96. 451
4 松本哲一、小林武彦 (1999) 御嶽火山、古期御嶽火山噴出物のK-Ar年代に基づく火山活動史の再検討.火山,44,1-12. Matsumoto, A. and Kobayashi, T. (1999) K-Ar Ages of the Older Ontake Volcanic Products, Ontake Volcano, Central Japan: Reappraisal of the Volcanic History Based on the Radiometric Data. Bull. Volc. Soc. Japan, 44, 1-12. (in Japanese with English Abstract) 552
5  Kioka, H., Furuyama, K., Miyake, Y., Sakai, J., Nagao, K., Ikemoto, M., Noiri, Hisayuki and Oda, K. (1998) K-Ar chronology of the Middle Pleistocene lavas at Ontake volcano, central Japan. Jour. Asso. Geol. Coll. Japan (Chikyu Kagaku),52,464-474. 46