地域地質研究報告
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6 40 D.I Matsuoka EPMA 63 9 EPMA EPMA ICP 76 Fig.1 Summary of geology in the Kitakomatsu district. Fig.2 Tectonic divisions in the Kitakomatsu district A No.940 Tricolocapsa plicarum Bajocian Bathonian iv -
7 * ** *** 9-11 * ** *** Keywords: areal geology, geologic map, 1:50,000, Kitakomatsu, Kyoto, Shiga, Lake Biwa, Hira mountain, Adogawa, Tamba, Permian, Triassic, Jurassic, Cretaceous, Quaternary, Pleistocene, Holocene, Tamba Belt, Sanyo Belt, accretionary complex, Type suite, Type suite, Haiya complex, Sasae complex, Yuragawa - complex, Furuya complex, Hanase-bessho quartz deorite, tonalite, Hira granite, Ryozen granodiorite, dikes, granitic porphyry, Kobiwako Group, terrace deposits, alluvium, active fault, Hanaore fault, Hira fault, Uedera fault, Manganese deposits, hot spring, radiolarian fossil - 1 -
8 135 45' 136 0' 35 10' 35 20' m - 2 -
9 m 1,000-1,200m 1,000m m m 1,000m
10
11 3 1000m 4 NE SW NW SE NE SW km
12 II I km 1983 Imoto Imoto km Ma K-Ar Ma K-Ar m m - 6 -
13 a 4b 4c 5 5a 5b 5c C 1998
14
15 6-9 -
16 km 1-10m/ km Sakaguchi a-l a 1979b Isozaki and Matsuda Imoto
17 Imoto tectonostratigraphic unit Nakae 1993 Yoshizawa et al Yoshida
18 Oceanic plate stratigraphy Taira et al Matsuda and Isozaki Nakae Imoto chert-clastics sequence Otsuka Kimura and Hori Kimura and Hori 1993 Isozaki Ma
19 Ma km
20 m 50m km 3 2
21 cm m km m 10-50m 50m 100m 200 m 400m 70m 400m 5km 30-70m 4 2 Nakae 1990 G-H 3km E W ENE WSW
22 m m 40m 20-50m m m 115m 400m 405m m m m
23 Nakae Nakae I I 1998 I I 1998 WNW ESE WNW ESE m 50m a
24 8 a b c d 15cm 20cm 5-15cm 8 b 5-10cm 8 c d
25 1 1-10cm 1mm 5cm 9 a 2-5cm 9 b 150m 30m 9 a b 30cm 10 a 1m b 15cm
26 m 10 a 10 b 1cm 11 a 11 a S1 b c d 15cm 6cm 18cm 30cm
27 10cm 11 b 11 c d 1994 C 3-20cm m 12 a b 15cm
28 12 a m 13 a b c d e E f 30cm 6cm
29 12 b 13 d e 5-20cm f 14 a b S1 a C 10m d 6cm 15cm
30 50-150cm 1-3cm 13 a 40m 13 b cm 13 C cm 14 a d
31 cm WNW ESE 80m 5m 5cm 10m 3-15cm
32 R1-R16 3 Matsuoka Matsuoka 1995 JR1-JR8 8 JR1-JR8 5 1 R1 R2 Tricolocapsa (?) fusiformis, T. Plicarum JR
33 2 gm bm
34 3 sil.ms ms ch tf A C M MG PM 4 R 15 R16 Zhamoidellum ovum Tricolocapsa yaoi JR7 JR8 R13 17 R4 12 stichocapsa naradaniensis Stylocapsa(?) spiralis, Gongylothorax sakawaensis JR6 R Tricolocapsa tetragona T. conexa JR5 R3 Tricolocapsa plicarum T. tetragona JR4 JR5 JR Neospathodus timorensis, Pollygnathus kochi
35 4 Matsuoka 1995 Neospathodus(?) homeri OG1 Pseudodictyomitra primitiva OG3 Gongylothorax sakawaensis
36 -Stichocapsa naradaniensis 93-3 Tricolocapsa yaoi 2 OG Stichocapsa naradaniensis Tricolocapsa conexa T. plicarum OG3 Guexella nudata
37 1997 Matsuoka 1995 JR Isozaki and Matsuda
38 JR I
39 R2 JR
40 4 7 D 1 D D1-D3 7 1 D 1 F1 imbricate thrust sole
41 b 50 cm-1.5m a S 1 14a b S 1 S 1 S 1 S
42 Ant. Syn
43 a b 7 2 D 2 S 2 D Ma Ma Isozaki and Matsuda km 1 18 D 2 30cm
44 S 2 45km 5-7km 2 400m-1.5km 3 1km 3 100m ß m S2 19 D cm 2 30cm
45 20 D 2 a b P Y 30 cm 15cm S1 S km 400m-1km 2 E W 60 5m 45m 4 P Y ENE WSW 10km 20m 20 a E W 30 P Y 20 b
46 21 S2 a b S 1 S1 6cm 16cm S 2 S 2 E W S2 S2 S a b S 2 S 1 S 2 S 1 S 2 12 b 21 c S
47 S2 S2 7 3 D 3 SW K-Ar Ma Shibata and Ishihara 1974 D cm a S 1 S a mm-1cm 22 a 65 S 1/S2 b 30cm 6cm
48 5-10cm NE SW NW SE 22 b Hd 1986 Yoshida km m 23 a NNE SSW NE SW 15-20m 20-30m NNE SSW 23 a b 30cm
49 km 1998 II m 1000m m m km 2000 II ESE E W NW SE WNW ESE 3 1-2m 2-10m 23 b ENE WSW NE WS ENE WSW 30km m 25m 10-50cm
50 Ishihara a b 4-5km 13km
51
52 2km km 2.5km 1.6km K-Ar Ma 2000 XRF Yoshizawa et al Uchiyama 1983 Yoshizawa et al
53 1997 Yoshizawa et al Uchiyama 1983 Yoshizawa et al Uchiyama XRF Yoshizawa et al XRF XRF G km 1.6km
54 26 a b mm 5mm b a-d c Z
55 27 G G U TK G 3 G 4 G 5 G G K-Ar Ma XRF 6 6 HA km 10m
56 e X Y Z Z 2000 XRF 6 2km 300m 250m f X Y Z Z 2000 XRF
57 28 a b c d e f P1 Q Bt Hb
58 3 3 Yoshizawa 1965 et al. 24 E W N60 W N60 W 4 1 G 3 2 G 4 3 G 5 4 G KT SI SI
59 29 a 2D-8 b 4G-8 C 2G-6 1 1mm cm
60 m cm m 1mm1mm 29 mm a b X Y Z 1997 XRF 7 800m 30 Pl Af Q
61 100m 1-5mm mm 1-2mm C-3 1 1mm cm 32 Pl Af Q
62 33 1 1mm cm a 1E-1 b 2B
63 a b X Y Z Ma K-Ar XRF 7 G mm 15mm 10mm 10mm 10mm 20mm 10mm cm 1-3mm a 37 b 3mm 2mm X Y Z Ma K-Ar XRF 7
64 34 a b a b 3G7 600m
65 cm
66 37 a b
67 1mm 38 5mm 1cm 38 3C-6 1 1mm cm 39 Pl Af Q
68 a b X Y Z 1997 XRF
69 8 EPMA
70 JXA8800M 15kV 0.2 A 5 m 50 m 8 Ab56 Ab40 Ab Ab93 Ab96 Ab Fe 1996 Ti Or EPMA
71 10 EPMA 3 Or Or83 D.I. 40 SiO D.I Aramaki et al K 2O Na2O SiO2 Al2O Or/Ab 3 4 Yoshizawa et al km 2km b Uchiyama
72 40 D.I Aramaki 1972 et al
73 41 500m 1 1mm cm X Y Z XRF m Yoshizawa et al
74 42 a b
75 XRF
76 4 2 3 ENE WSW 5 2 cm 43 a b NE WS Ma K- Ar a b c d Pl Q
77 XRF 12 N5 20 E N 5-30mm N30 W 58 S 200m 1982 XRF m km NNE SSW 44 5mm 45 Yoshizawa et al SiO c d 1997 XRF 12 2 SiO D.I
78 44 45cm
79 SiO2 Al2O 3 CaO K 2O Na2O FeO MgO 40 Qz-Ab- Or An-Ab -Or An Rb Sr Rb Sr 2000 Rb Sr 1976 Sr Sr SW NW K-Ar Ma K-Ar
80 Rb-Sr 57.4Ma km m
81 m m cm Ma FT cm
82 ICP
83 m Stegodon akashiensis Kamei 1966 Manmmuthus paramenmmonteus shigensis I 0.9Ma Ma Nishimura and Yokoyama Yokoyama et al Yokoyama et al., m 80 Yokoyama et al Menyanthes 1980 BB195 Biwa
84 2 I III I IV I m ps
85 4 t ,000m 50m 5 a am ab al af am ab al af 2.4m 2m Tn AT
86 1 1 1) km m up-hill I A 1-10m / m , )
87
88 km km )
89
90 Co II /
91 1 Imoto
92 Mn Mn45.05 MnO Fe 1.68 SiO P 0.08 S 0.01 Mn29.37 Fe 1.95 CO P 0.11 S m 65m 0.35m 3.0 2,048 2,700 3km 750m 3 Mn MnO Fe 3.24 SiO P 0.07 S m 8m 0.35m Mn t m
93
94 6.7 /m 1,000mg/kg Rn /m ph mg/kg 8.25 Rn /m ph mg/kg Rn m 400m
95 Aramaki, S., Hirayama, K. and Nozawa, T. (1972) Chemical compositions of Japanese granites, Part 2. Variation trends and average compositions of 1200 analyses. Jour. Geol. Soc. Japan, vol.78. D p vol p p 1960 no.1 p p Imoto, N. (1984) Late Paleozoic and Mesozoic cherts in the Tamba Belt, Southwest Japan. Bull. Kyoto Univ. Education, vol.65, p p p 1982 no.92 p vol.89 p vol.39 p Ishihara, S. (1977) The magnetite-series and ilmenite-series granitic rocks. Mining Geology, vol. 27, p vol.9 p Isozaki, Y. (1997) Jurassic accretion tectonics of Japan. The Island Arc, vol.6, p Isozaki, Y. and Matsuda.T. (1980) Age of the Tamba Group along the Hozugawa Anticline", Western Hills of Kyoto, Southwest Japan. Jour. Geosci., Osaka City Univ., vol.23, p Ku6C co -ignimbrite ash- vol.100 p
96 Kamei, T. (1966) Notes on Elephas shigensis (Matsumoto and Ozaki) from the Osaka Group and Paleo-Biwa Group. Mem. Fac. Sci. Univ. Kyoto, ser. B, vol.32, p p 1970 MAGMA no p vol.79 p MAGMA no.78 p MAGMA no.81 p K- Ar vol.101 p vol.29 p MAGMA no.86 p vol.34 p out-of-sequence thrust no.50 p no.55 p Kimura, K. and Hori, R. (1993) Offscraping accretion of Jurassic chert-clastic complexes in the Mino-Tamha Belt, central Janan. Jour. Struct. Geol., vol.15, p p p p p 1992 vol.31 p p p
97 3 vol.45 p p 1985 p.274p Matsuda, T. and Isozaki, Y. (1991) Well-documented travel history of Mesozoic pelagic chert in Japan: from remote ocean to subduction zone. Tectonics, vol.10, p Matsuoka, A. (1995) Jurassic and Lower Cretaceous radiolarian zonation in Japan and in the western Pacific. The Island Arc, vol.4, p vol.90 p no.34 p p p vol.71 p no.303 p p Nakae, S. (1990) Melanges in the Mesozoic sedimentary complex of the northern part of the Tamba Belt. Jour. Geol. Soc. Japan, vol.96, p Nakae, S. (1993) Jurassic Accretionary Complex of the Tamba Terrane, Southwest Japan, and its formative Process. Jour. Geosci., Osaka City Univ., vol.36, p no.55 p p vol.10 p p Nishimura, S. and Yokoyama, T. (1975) Fisshon-track ages of volcanic ashes in core samples of Lake Biwa and Kobiwako Group (2). Horie, S. ed., Paleolimnology of Lake Biwa and Japanese Pleistocene, vol.3, p
98 1985 vol.9 p Otsuka, T. (1988) Paleozoic-Mesozoic sedimentary complex in the eastern Mino Terrane, central Japan, and its Jurassic tectonism. Jour. Geosci. Osaka City Univ., vol.31, p p 1982 p vol.8 p Sakaguchi, S. (1961) Stratigraphy and paleontology of the south Tamba District,part 1, Stratigraphy. Mem. Osaka Gakugei Univ., ser. B, vol.10, p Sakaguchi, S. (1963) Stratigraphy and Palaeontology of the South Tamba District, Pt., Palaeontology. Mem. Osaka Gakugei Univ., ser. B, vol.12, p vol.22 p no.390 p vol.51 p K-Ar vol.99 p vol.100 p p vol.88 p vol.44 p vol.51 p vol.54 p Shibata, K. and Ishihara, S. (1974) K-Ar ages of the tungsten and molybdenum deposits in Japan. Econ. Geol., vol.69, p p
99 no.18 p no.10 p vol.31 p vol.81 p Sr no.53 p Taira, A., Tokuyama, H. and Soh, W. (1989) Accretion tectonics and evolution of Japan. In Ben Avraham, Z., eds., The Evolution of the Pacific Ocean Margins. Oxford University Press, New York, p p p p vol.23 p vol.25 p vol.28 p vol.33 p a 4 vol.33 p b5 vol.33 p vol.34 p I vol.44 p no.25 p Uchiyama, E. (1983) Plutonic rocks in the Hira mountain range. Abstracts of Master Thesis, Div
100 Educ., Grad. Cour., Kobe Univ., p p vol., Yao, A. (1990) Triassic and Jurassic radiolarians. In Ichikawa, K., Mizutani, S., Hara, I., Hada, S. and Yao, A., (eds.), Pre-Cretaceous Terranes of Japan. IGCP Project No.224, Osaka, p vol.19 p Yokoyama, T., Nakagawa, Y., Takemura, K., Mori, S., Makinouchi, T., Hayashida, A., lida, Y. and Matsuoka, K. (1979) Stratigraphy of the Takashima Formation of the Plio-Pleistocene Kobiwako Group, Japan. In Horie, S. ed., Paleolimnology of Lake Biwa and Japanese Pleistocene, vol.7, p Yokoyama, T., Takemura, K. and Matsuoka, K. (1977) Preliminary report on the Takashima Formation, uppermost part of the Kobiwako Group, Plio-Pleistocene sediments around Lake Biwa, Japan. In Horie, S. ed., Paleolimnology of Lake Biwa and Japanese Pleistocene, vol.5, p no.2 p p Yoshida, S. (1986) Hanaori Fault, a left-lateral strike-slip fault, northeast of Kyoto. Jour. Fac. Sci. Univ. Tokyo, sec., p no.489 p p 1969 vol p 1998 no.37 p vol.99 p vol.59 p p vol.51 p Yoshizawa, H., Ishizaka, K., Kaneko, K. and Kawahara, M. (1965) Geology and petrography of the Hira Granite, and mutual realtions between granites in the northeastern Kinki district, Japan. Mem. Coll. Sci. Univ. Kyoto, Ser. B, vol.31,
101 QUADRANGLE SERIES SCALE 1: 50,000 Kyoto (11) No.16 GEOLOGY OF THE KITAKOMATSU DISTRICT By Katsumi KIMURA, Toshikazu YOSHIOKA, Satoshi NAKANO and Atsushi MATSUOKA Written in 2000 ABSTRACT The Kitakomatsu district is situated in both the eastern part of Kyoto Prefecture and the western margin of Shiga Prefecture. The geologic province of the area belongs to the Tamba Belt in the Inner Zone of Southwest Japan. The Tamba Belt consists of Jurassic accretionary complexes, which were intruded by Cretaceous granitic rocks and dikes, and covered unconformably by the Pleistocene Kobiwako Group, terrace deposits and alluvium. Figures 1 and 2 show a summary of the geology and tectonic division of the Kitakomatsu district, respectively. MESOZOIC Accretionary complex of the Tamba Belt The Tamba Belt is underlain by Jurassic accretionary complexes, consisting mainly of Jurassic terrigenous rocks and older oceanic material such as basaltic rocks, limestone, Toisihi-type siliceous mudstone, and bedded chert. The age and stratigra
102 Fig. 1 Summary of geology in the Kitakomatsu district
103 Fig. 2 Tectonic divisions in the Kitakomatsu district.
104 phic relationship of these rocks allow us to reconstruct an oceanic plate stratigraphy; that is, in ascending order, basalt rocks, limestone, bedded chert, siliceous mudstone, black mudstone, and sandstone. The youngest age of the terrigenous rocks may indicate the age of accretion onto an accretionary prism by subduction processes. The Jurassic accretionary complexes in the Tamba Belt, is divided into six tectonostratigraphic units, based mainly on age and lithology of the oceanic plate stratigraphy, which are structurally from top to bottom, named the Shuzan, Kumogahata, Haiya, Sasae (Tsurugaoka), Furuya and Yuragawa Complexes. Each complex is bounded by a thrust fault. Except for the Furuya Complex, the age of the clastic rocks, siliceous mudstone and bedded chert of each complex is younger structurally towards the bottom. The former three complexes form the major unit named the Type Suite, characterized by Permian bedded chert and limestone underlain by basaltic rocks, while the later three complexes constitute the Type Suite, characterized by Triassic to Jurassic bedded chert underlain by Lower Triassic Toishi-type siliceous mudstone without significant Permian rocks. Both suites are separated by the Haiya Thrust. The Haiya and Kumogahata Complexes are not distributed in the Kitakomatsu district. The Jurassic accretionary complexes are folded to form the Hatcho Antiform which plunges westward in the Kitakomatsu district. The Haiya Complex occupies a small area in the southwestern corner of the district and only includes greenstone and mixed rock. The Sasae and Yuragawa Complexes are distributed widely in the district, which are characterized by a stacked pile of more than 4 thrust sheets composed of an oceanic plate stratigraphy including in ascending order, Toishi-type siliceous mudstone, bedded chert, siliceous mudstone, greenish gray mudstone, black mudstone with intercalations of interbedded sandstone and mudstone. The Sasae Complex differs from the Yuragawa Complex in the lithology with great amounts of mixed rock including greenstone. The Furuya Complex is distributed in the northern margin of the district. Although the stratigraphic sequence has not been confirmed by fossil age data, it appears to be characterized by a coherent sequence including in ascending order, bedded chert, siliceous mudstone, greenish gray mudstone, black mudstone and interbedded sandstone and mudstone. Granitic rocks and dikes Granitic rocks are distributed widely in the eastern part, and sporadically in the western part of the Kitakomatsu district. The granitic rocks belong to the San'yo Belt, one of the granitic petrographic provinces in Southwest Japan. These rocks are subdivided into the Hanase-bessho quartz diorite, small tonalitic bodies, Hira granite and Ryozen granodiorite, based on their occurrence, petrographic characteristics and radiometric age. The granitic rocks are intruded into the Type suite of the Tamba Belt. Strata surrounding the granitic rocks have undergone thermal metamorphism forming biotite and rare cordierite. The isotopic ages of the granitic rocks range from 70 to 100 Ma
105 The dikes are intruded into the strata of the Tamba Belt and granitic rocks. The dikes are divided into three rock types: mafic rocks, granite porphyry and rhyoritic dacite. The first type includes gabbro, hornblende porphyrite and diorite porphyry. The second type includes granite quartz porphyry and aplite. CENOZOIC Pleistocene Kobiwako Group In the Kitakomatsu district, the Kobiwako Group is distributed in the hilly area surrounding the Hira Mountains and Lake Biwa. The Kobiwako Group includes the Hata, Katata and Takashima Formations, consisting of fluvial and lacustrine gravel, sand, and mud with intercalations of tephra. Terrace deposits and alluvium The terrace deposits are mainly distributed in the Katata Hill and Taizanjino plateau and along some large rivers. These terraces are divided into the following: Higher, Middle, and Lower to. The Middle terraces were formed during the last interglacial age. These terrace deposits are composed mainly of gravel and sand. Alluvium is widely distributed on the western side of Lake Biwa, and consists of gravel, sand and mud. Active faults There are several active faults in this district. The Hanaore Fault is a right-lateral strike-slip fault that trends NNE-SSW for a distance of 48 km. Paleoseismological studies show that the last faulting occurred after 15th Century. There are the Hira, Haido and Kamidera Faults along the western shoreline of Lake Biwa. They are reverse faults which have uplifted the Hira Mountains. ECONOMIC GEOLOGY In the Kitakomatsu district there are many manganese ore deposits, one working quarry, and three hot springs. The manganese ore deposits are embedded in the bedded chert of the Yuragawa Complex of the Tamba Belt. All mines have been closed. There are three hot springs in the mapped district, which are classified into two types of springs, that is, simple and radioactive springs according to their respective water chemistry. Their chemical characteristics are related to the local geology
106 A 1 1/50,000 8 R
107 /50,000
108 No.940 Tricolocapsa plicarum Bajocian-Bathonian 375 R1 1. Tricolocapsa plicarum Yao 2. Tricolocapsa(?) fusiformis Yao 3. Tricolocapsa sp. cf. T. ruesti Tan 4. Protunuma fusiformis Ichikawa and Yao 5. Eucyrtidiellum sp. aff. E. unumaense (Yao) 6. Archaeodictyomitra suzukii Aita 7. Dictyomitrella (?) kamoensis Mizutani and Kido 8. Hsuum robustum Pessagno and Whalen 9. Spongocapsula yehae Pessagno, Blome and Hull
109 p BIBLIOGRAPHIC REFERENC Kimura, K., Yoshioka, T., Nakano, S. and Matsuoka, A.(2001) Geology of the Kitakomatsu district. With Geological Sheet Map at 1:50,000, Geol.Surv Japan, 102p. (in Japanese with English abstract 5p.).
Occurrence of Permian radiolarians from chert pebbles in conglomerate at Yokoo, Nyukawa Village, Gifu Prefecture, central Japan Satoru KOJIMA* Abstrac
Occurrence of Permian radiolarians from chert pebbles in conglomerate at Yokoo, Nyukawa Village, Gifu Prefecture, central Japan Satoru KOJIMA* Abstract Permian Radiolaria including Albaillella levis, Follicucullus
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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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地域地質研究報告
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Mesozoic Radiolarian Terranes (MRT) of Southwest Japan Koichiro ICHIKAWA* Abstract In contrast to Molluscan terranes which are composed of shallow - w
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Makoto Saito and Kazuhiro Miyazaki (2006) Jadeite-bearing metagabbro in serpentinite melange of the Kurosegawa Belt in Izumi Town, Yatsushiro City, Kumamoto Prefecture, central Kyushu. Bull. Geol. Surv.
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5 1 11 41 NI-53-8-15 15 5 1 Index of the Geological Map of Japan 1 50,000 * ** *** + ++ +++ ++++ 1882 5 1 1978 8 1979 5 11-13 1980 1982 14 * ** *** Keywords geologic map 1 50 000 Minakuchi Shiga Kyoto
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Nobuharu Hori (2004) Jurassic radiolarians from chert and clastic rocks of the Chichibu Belt in the Toyohashi district, Aichi Prefecture, Southwest Japan. Bull. Geol. Surv. Japan, vol. 55(9/10), p.335-388,
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5 Report on the Landslide Disaster in the Upper Part of the Abukuma River, Fukushima Prefecture, Due to Heavy Rainfall in August 1998 By Takashi INOKUCHI National Research Institute for Earth Science and
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Kazuhiro Miyazaki (2003) Tentative standardized legends of metamorphic rocks for 1/200,000 scale seamless geological map of Japan. Bull. Geol. Surv. Japan, vol. 54(9/10), p.295-302, 2 figs. Abstract: This
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