地域地質研究報告
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1 550.85(084.32) (521.11) 1 50,000 (083)
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10 6 2.5km 1.7km 1,625.2m mudflow hill m
11 ,400m 200m 400 1,200m m 7 2
12 m 45m , m 600 1,000m m 200 1,400m m m N-S NNW-SSE 8 N-S N NNW-SSE NNE-SSW SK SK-1 NS
13 9 NS m m 45m m m 45m m ,000m m 200 1,400m NS NNW -SSE m 150m 250m m SK-1 2.5m m 0.1m 1 2 l954
14 10 2m Sagarites (Makiyama) chitanii (MAKIYAMA) 1962 Martinottiella communis, Bathysiphon sp. Cyclammina japonica, Goesella sp., Haplophragmoides trullissatum, H. renzi, Massilina sp., Spirosigmoilinalla compressa m 600 1,000m 45m 0.1m m cm Sagarites (Makiyama) chitanii (MAKIYAMA) 1962 Bathysiphon sp., Cyclammina japonica, C. pusilla, Haplophragmoides, Spirosigmoilinella compressa 1966 Lucinoma acutilineatum (CONRAD) Epistominella, Haplophragmoides, Martinottiella, Spirosigmoilinella, Globigerina
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17 m m m 0.1 3m 10 15cm Sagarites Makiyama chitanii MAKIYAMA Eggerella sp., Martinottiella sp., Miliammina echigoensis ASANO and INOMATA Conchocele sp
18 m cm 10cm 2 4m SK-1 20m 20m 70m Dentalium weinkauffi DUNKER Acila nakazimai OTUKA Nuculana cf. sadoensis YOKOYAMA Dentalium weinkauffi DUNKER Nuculana cf. sadoensis YOKOYAMA Limopsis sp. Pododesmus macroschisma DESHAYES
19 15 Septifer sp. Clinocardium cf. californiense DESHAYES Ezocallista cf. brevisiphonata CARPENTER Macoma nipponica TOKUNAGA Acila nakazimai OTUKA Nuculana cf. sadoensis YOKOYAMA Macoma nipponica TOKUNAGA Dentalium weinkauffi DUNKER Elphidium-Cibicides
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21 m 10 20m 6.0km SK m m pyroclastic flow deppsit ash flow m 150m 1958 Menyanthes trifoliata LINNE 9 1 2
22 km m m 276m 50m 1 2 Vd mm mm mm m 8 Vd
23 mm mm Vd mm mm mm 10 3 Vd mm 3.0mm mm mm Vd mm mm mm ,625.2m NW-SE 800m NE 3
24 20 -SW550m 1961 d mm 1.0mm V cz 45 Wo 43 En 38 Fs 19 Wo 42 En 32 Fs mm Fs mm mm X Y Z cz 0 min mm mm 10 5 air fall pyroclastic deposits 2 A 65km 2 20m 1.3km m 500m 700m 145m 300m
25 7 21
26 (humus) m 0.7km 3 0.6km m 0.5m 1.5m NS td Sd
27 vol , vol 55 no vol 55 no vol 12 no 3 11 IWAI T 1960 Pliocene Mollusca from the Nishi-tsugaru District, Aomori Prefecture, Japan. Saito Ho-on Kai Museum Research Bulletin, no no IWAI, T The Geological and Paleontological Studies in the Marginal Area of the Tsugaru Basin, Aomori Prefecture, Japan. Bulletin of Educational Faculty of Hirosaki University, no no vol 27 no 6 16 KANAYA, T Miocene diatom assemblages from the Onnagawa formation and their distribution in the correlative formations in northeast Japan. Sci. Rep. Tohoku Univ., 2d ser. Geol., vol
28 vol 60 no KAWANO, Y., Yagi, K. and Aoki, K Petrography and petrochemistry of the volcanic rocks of Quaternary volcanoes of northeastern Japan. Sci. Rep. Tohoku Univ., Ser. III, vol. 7, no vol 46 no no no KUNO H 1962 Catalogue of the active volcanoes of the world including solfatara fields. Part XI. Japan. Taiwan and Marianas, International Association of Volcanology, Rome Bouguer no vol 13 no vol 15 no vol 16 no vol 12 no
29 25 MS vol vol 69 no vol 10 no 3 vol 13 no no no 48
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31 1 QUADRANGLE SERIES SCALE 1: 50,000 Aomori 5 No. 21 GEOLOGY OF THE GOSHOGAWARA DISTRICT By Atsushi OZAWA and Jiro HIRAYAMA (Written in 1969) (Abstract) GEOLOGY The mapped area is located in the western part of the Aomori Prefecture, Northeast Japan. The stratigraphic sequence of the area is summarized in Table 1.
32 2 Table 1 NeogeneTertiary The Neogene Tertiary may be divided into so-called Green Tuff and Oil Tertiary of Northeast Japan. The former is characterized by greencolored volcanic rocks and includes the Kuroishizawa Formation. The latter is characterized by sedimentary rocks with a small amount of volcanics, and includes the Odoji, Akaishi, Maido, Narusawa and Tatsuyama Formations. Kuroishizawa Formation (thickness 400m ) The Kuroishizawa Formation, the lowermost of the Neogene Tertiary in the mapped area, is divided into the lower and upper parts, and the lithofacies of each part is shown as follows. Lower part (thickness 150m ) : Basalt tuff breccia, lapilli tuff and tuff. Upper part (thickness 250m ) : Andesite tuff breccia and lapilli tuff.
33 3 Odoji Formation (thickness m) The Odoji Formation overlies the Kuroishizawa Formation with unconformity. It consists of hard shale and acid tuff. Akaishi Formation (thickness m) The Akaishi Formation conformably overlies the Odoji Formation and consists of black mudstone. Maido Formation (thickness m) The Maido Formation overlies the Akaishi Formation with conformity, and consists of silty mudstone. Narusawa Formation (thickness m) The Narusawa Formation overlies the Maido Formation with conformity, and consists chiefly of sandstone, associated with acid tuff. Tatsuyama Formation (thickness m) The Tatsuyama Formation overlies the Narusawa Formation with conformity, and consists of sandstone and acid tuff. The mapped area is characterized by the folded structure with a general trend of N-S to NNW-SSE direction. From west to east, the Narusawa syncline, Morita anticline and Goshogawara anticline are successively arranged. The anticline coincides with the positive gravity anomaly and the syncline with the negative. The remarkable change in thickness of the Neogene deposits is recognized between the sites of Narusawa syncline and Morita anticline. On the western side of the boundary, the Akaishi Formation is 200 to 600m in thickness, and the Maido Formation is 150 to 600m. On the other hand, on the eastern side of the boundary, the Akaishi Formation is less then 45m in thickness, and the Maido Formation is 30 to 100m. Quaternary The Quaternary rocks comprise Iwaki volcano, the Diluvial deposits and the Alluvium. Iwaki volcano occupies the southwestern part of the mapped area. It has an elliptical caldera 1.7km and 2.5km in diameter. The somma is composed of hypersthene-augite andesite lava, olivine-hypersthene-augite andesite lava and their pyroclastics.
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地質図幅説明書
550.85(084.32)(521.77)[1 50,000](083) 109 40 ... 1... 5 1... 5 2... 7 2 1... 7 2 2... 10 3... 14 3 1... 14 3 2... 19 3 3... 22 4... 23... 23 1... 23 2... 24... 24 Abstract... 1 1 1 50,000 39 109 38 22
地域地質研究報告
550.85(084.32)(522.8)[1:50,000](083) 5 1 (15) 80 46 1 4 1 4 2 5 3 5 4 7 5 10 6 11 7 13 8 13 9 15 10 16 11 19 12 20 13 21 14 21 21 1 21 2 22 3 24 4 25 5 26 6 26 7 27 27 Abstract 1 1 5 1 15 80 43 41 4270
地域地質研究報告
(1) (2, 3) (4) (5) (6,7,8,9) 2 (Ma) s (Ns) i (Ni) d (Nd) Pr (2 ) Age1 (cm -2 ) (cm -2 ) (10 4 cm -2 ) r (%) (ppm) 1ED1ED2 6T=(1/n1+ ( (ED1 s 1/2 2NIST-SRM612 7 t =T1/Ns+1/Ni+1/Nd+ ( / 2 1/2 3JRR-3 4r s
地質図幅説明書
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No. 35 (2000) pp.115-124 The Late Quaternary stratigraphy in the western margin of Yodobashi- dai, northern part of Setagaya-ku, Tokyo Jiro KOMORI, Kunihiko ENDO, Fumihiko HASEGAWA, and Sei TAMURA (Received
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29 28 39 1936 Acquiring technique and forming character in physical education after 1936 Analysis of articles of Kenji Shinozaki FUJIKAWA Kazutoshi The United Graduate School of Education Tokyo Gakugei
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Japanese Civilian Control in the Cold War Era Takeo MIYAMOTO In European and American democratic countries, the predominance of politics over military, i.e. civilian control, has been assumed as an axiom.
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Study on the System of the Chinese Autistic in Japan Xiaotong Ro abstract This study note is mainly introduced the research of China s autistic child treatment in Japan. There is not very much research
* ** Casualties by the 3 June 1991 pyroclastic flow at Unzen volcano Shinichi SUGIMOTO * and Daisuke NAGAI ** Abstract The eruption of Unzen
九州大学学術情報リポジトリ Kyushu University Institutional Repository 雲仙火山 1991 年 6 月 3 日の火砕流による人的被害 杉本, 伸一島原市役所島原半島ジオパーク推進室 長井, 大輔九州大学大学院理学研究院附属地震火山観測研究センター https://doi.org/10.15017/13523 出版情報 : 九州大学大学院理学研究院研究報告.
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Yoshio UEDA Bouguer anomalies decrease step-wisely toward the inner arc, showing two sharp gradient zones to the east of the volcanic front. The acros
REPORT OF HYDROGRAPHIC AND OCEANOGRAPHIC RESEARCHES No.41 March, 2005 Abstract The Hydrographic and Oceanographic Department of Japan have been conducted marine gravity surveys since 1965. Based on theses
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LAGUNA8 67 78 2001 3 LAGUNA 8 p.67 78 2001 1 1 2 3 4 5 6 7 8 Saline wedge at River Gonokawa, Shimane Pref., Japan Saline water intrusion at estuary river and its relation to the underground water Observation
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20 * Re-Evaluation of Isoseismal Maps and Magnitudes from Two Big Earthquakes along the Subduction Zone of Kyushu and Ryukyu Islands Early in the 20th Century Masayuki TAKEMURA, Katsuhisa KANDA Kobori
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LAGUNA 33 6 7 LAGUNA p.33 6 7 Rising water level events in the Ohashi River, Shimane Prefecture. Kengo Kurata Abstract: Several periods of water level rise in the Ohashi River, Shimane Prefecture were
Sport and the Media: The Close Relationship between Sport and Broadcasting SUDO, Haruo1) Abstract This report tries to demonstrate the relationship be
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Rolly E. RIMANDO *** Jessie DALIGDIG *** Arturo DAAG *** Surface Faulting Associated with the Philippine Earthquake of 1990 Takashi NAKATA *, Hiroyuki
Rolly E. RIMANDO *** Jessie DALIGDIG *** Arturo DAAG *** Surface Faulting Associated with the Philippine Earthquake of 1990 Takashi NAKATA *, Hiroyuki TSUTSUMI**, Raymundo S. PUNONGBAYAN ***, Rolly E.
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The Regional Structure of Car Industry in China Yoshiyuki KITAMURA 1 1956 2 20051979 1980 20 1990 2006 1993 19982003a2000 2005 2003200421 2003 3 2,037,865 4,443,52245.92,443 115 129 43-22005 1436382,149,693
19 Figure-2 General Layout of Mahaica-Mahicony-Abary Lower River Basin Rural Development Plan Study Location Map of Cooperative Republic of Guyana PROJECT DIGEST 1. PROJECT TITLE : Mahaica-Mahaicony-Abary
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SEISMIC HAZARD ESTIMATION BASED ON ACTIVE FAULT DATA AND HISTORICAL EARTHQUAKE DATA By Hiroyuki KAMEDA and Toshihiko OKUMURA A method is presented for using historical earthquake data and active fault
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Topographical and geological characteristics of Sofugan Tectonic Line (STL) area, Izu-Ogasawara Arc. Izumi SAKAMOTO Toshiya FUJIWARA and Osamu ISHIZUKA Sofugan Tectonic Line STL locates on the middle part
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Prognostication of Success in Sumo-Wrestler Appricants AKIYOSI SUDA About 320 Sumo wrestler appricants were divided into two groups a superior group (Makushita and Sandanme class) and an inferior group
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*1 Study on Room ressure Control at Cleanroom art 1 Experiments on Room ressure Fluctuation with Door Operation and Local Ventilation Operation Yukitada MURAE *1 Tamio IWAMURA *2 Hiroyuki NAGAI *3 Shigeru
Title 泌尿器科領域に於ける17-Ketosteroidの研究 17-Ketosteroidの臨床的研究 第 III 篇 : 尿 Author(s) 卜部, 敏入 Citation 泌尿器科紀要 (1958), 4(1): 3-31 Issue Date URL
Title 泌尿器科領域に於ける17-Ketosteroidの研究 17-Ketosteroidの臨床的研究 第 III 篇 : 尿 Author(s) 卜部, 敏入 Citation 泌尿器科紀要 (1958), 4(1): 3-31 Issue Date 1958-01 URL http://hdl.handle.net/2433/111559 Right Type Departmental Bulletin
* Meso- -scale Features of the Tokai Heavy Rainfall in September 2000 Shin-ichi SUZUKI Disaster Prevention Research Group, National R
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The Bulletin of the Institute of Human Sciences, Toyo University, No. 7 The Semantic Role and Function of GA and WO as object markers in Japanese WANG Yaxin The purpose of this paper is to analyze the
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56 1 19 Bull. Nara Univ. Educ., Vol. 56, No.1 (Cult. & Soc.), 2007 115 19 Why is Kidney Dysfunction Caused by Cadmium (Cadmium Nephropathy) not Officially Recognized as a Pollution-related Disease by the