Fig.. Geologic map showing distribution of the Takanoobane rhyolite lava and drilling sites AVL1-4. Distribution of lavas is after Ono and

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1 Jour. Geol. Soc. Japan, Vol. 111, No. 10, p , October 2005, Internal structures of the Takanoobane Rhyolite Lava in the western part of Aso caldera, Japan Abstract Kuniyuki Furukawa and Hiroki Kamata * Graduate School of Human and Environmental Studies, Kyoto University, Yoshida Nihonmatsu-cho, Sakyo-ku, Kyoto , Japan. Corresponding author: K. Furukawa, This study describes volcanic structures of four drilling cores obtained from the Takanoobane rhyolite lava distributed in Aso caldera, Japan and discuss on development of the structures of the lava. The Takanoobane lava is divided into three parts: Alternation of the pumiceous layers and the obsidian layers the upper part, the crystalline rhyolite layer the central part, and the obsidian layer the lower part. This variation of internal structures is interpreted to have been formed as a result of cooling and degassing processes during flowage. The central crystalline rhyolite layer contains many minute cavity parts defined as crystalline with many minute cavities. The minute cavity parts were formed immediately before or after the extrusion. At distal drilling site, the minute cavity parts were flattened and show flow layering. The flow layering shows high tilt angle in upper part of the crystalline rhyolite layer, suggesting a ramp structure. Key words: rhyolite lava, drilling core, structure, obsidian, spherulite, Aso caldera 1983 Inyo Drilling Program Eichelberger et al., 1984, , 1991 Aso-4, Manley and Fink, 1987; Dadd, 1992;, 1983 Manley, 1992; Fink et al, 1992, 1983, km, 1985 Fig km 3 SiO2 72, 2004 K-Ar 5, ka, ACP3:, 2003, 2003, AVL1-AVL Fig. 1 AVL4 120 m AVL1 230 m AVL2 340 m AVL3 380 m AVL m 200 m AVL m 160 m AVL m 145 m AVL m 200 m 4 AVL m CThe Geological Society of Japan

2 Fig.. Geologic map showing distribution of the Takanoobane rhyolite lava and drilling sites AVL1-4. Distribution of lavas is after Ono and Watanabe 1985 and Miyabuchi et al Fig.. Sections of the Takanoobane rhyolite lava in drill holes AVL m 91 m m 16.6 m m 54.5 m m AVL4, 2004 AVL1-AVL4 AVL1 -AVL4 Fe-Ti mm mm Miyagi et al., 1998; Miyagi and Matsubaya, 2003 Fe-Ti mm Fe-Ti mm

3 Fig.. Representative core samples from AVL1. A Finely vesicular pumice 14 m below the surface. B Coarsely vesicular pumice 20 m below the surface. C Upper obsidian 18 m below the surface. D Lower obsidian 94 m below the surface. E Crystalline rhyolite 42 m below the surface. AVL1 AVL4 Fig. 2 AVL AVL AVL1 AVL2 AVL m 2.5 m 5 m 0.01 mm mm Fig. 3A mm Fig. 3B 2.. Fig. 3C 3 4 m 5 m 3 m 0.01 mm 3 5 mm Lofgren, 1971a, b 40 cm Fig. 4A 13 m Fig. 3D 3 m cm.. 60 m Fig. 3E 0.01 mm 0.3 cm 5 cm Fig. 5

4 Fig.. A Core samples from AVL m in altitude showing the transition part between the coarsely vesicular pumice layer and the obsidian layer. B Core samples from AVL m in altitude showing the lower transition part between the crystalline rhyolite layer and the obsidian layer. The white arrows indicate spherulites. Fig.. Photograph A and sketch B of the cross-section surface of crystalline rhyolite from AVL1 50 m below the surface. Arrow indicates the upper direction of the lava. Dark color part and light color part in sketch indicate vapor phase mineral part and the minute cavity part, respectively. Fig.. Photomicrographs of the boundary between the crystalline rhyolite layer upper part and the minute cavity part lower part. A Under crossed polarized light. B Under reflective light. Dark color spots that do not reflect the light are minute cavities. Fig. 5B Fig. 6A Fig. 6B Obsidian Cliff Iddings, 1887 AVL m 5 cm 2 cm Fig. 7A 25 m m 0 20 Fig. 2 AVL m 1 cm 6 cm Fig. 7B AVL1

5 Fig.. Photographs and sketches showing shape of the minute cavity part grey part in sketches within crystalline rhyolite layer. A AVL1; lens shape B AVL2; stretched shape C AVL4; stubby or contorted shape. Fig.. Spherulitic structures from AVL4. A Spherulites showing light colors are abundant in the lower obsidian layer 29 m below the surface. B Photomicrograph, under plane polarized light, showing flow structure that passes through the spherulite without deflection. 10 m m m 0 20 Fig m cm Fig. 4B m 1 30 cm 7 m 1 10 cm AVL AVL3 Fig cm 3 m AVL AVL4 Fig m 3 m AVL1 AVL mm 4 m 1 40 cm 20 m AVL1 AVL2 AVL1 AVL2 Fig. 7C 30 m

6 m 1 cm Fig. 8A Fig. 8B Vernon 2004, Fig m 1 40 cm Cas and Wright, , 2001 Watanabe and Katsui, 1976, 2001, 2001 AVL1-AVL4 Skilling et al., Inyo Obsidian Dome Fig. 9A Fink and Manley 1987 Manley and Fink 1987 Fig.. Schematic columns of A a small to moderate volume subaerial rhyolitic lava, B a large-volume subaerial rhyolitic lava, and C a rhyolitic sill. These schematic columns are modified from Orth and McPhie Fink et al Sparks, 1978 AVL1 AVL2 AVL4

7 Fig.. Simplified schematic cross section showing horizontal variation of the minute cavity part. The minute cavity part is in stubby shape near the vent, and is stretched at distal sites... Obsidian Cliff Iddings, AVL4 AVL1 AVL Fig. 10 AVL3 3 AVL4 AVL4 AVL1 AVL2 AVL1 AVL2 Allen, 1936; Christiansen and Lipman, Manley and Fink, 1987 Manley and Fink, 1987 Ryan and Sammis, 1981 AVL3 AVL1 AVL2 Inyo Obsidian Dome, 50 m;, km 3 ; Orth and McPhie, 2003 Manley and Fink, 1987 Fig. 9A Snake River Plain, m;, 10

8 km 3 Bonnichsen and Kauffman, 1987 Fig. 9B Onedin 50 m Inyo Obsidian Dome Orth and McPhie, 2003 Fig. 9C, 90 m;, 0.14 km 3 Inyo Obsidian Dome Snake River Plain Onedin Inyo Obsidian Dome 8 Snake River Plain Onedin Orth and McPhie 2003 Inyo Obsidian Dome Vogel et al., 1987 Swanson et al., 1989 Hausback, 1987 SiO4 Lofgren, Inyo Obsidian Dome 4 15 Allen, J. E., 1936, Structures in the dacitic flows at Crater Lake, Oregon. Jour. Geol.,, Bonnichsen, B. and Kauffman, D.F., Physical features of rhyolite lava flows in Snake River Plain volcanic province, southwestern Idaho. Geol. Soc. Am. Spec. Pap.,, Cas, R. A. F. and Wright, J. V., 1987, Volcanic successions, modern and ancient. Academic Division of Unwin Hyman Ltd, London, p528. Christiansen, R. L. and Lipman, P. W., 1966, Emplacement and thermal history of a rhyolite lava flow near Fortymile Canyon, Southern Nevada. Geol. Soc. Am. Bull.,, Dadd, K. A., 1992, Structures within large volume rhyolite lava flows of the Devonian Comerong Volcanics, southern Australia, and the Pleistocene Ngongotaha lava dome, New Zealand. Jour. Volcanol. Geotherm. Res.,, Eichelberger, J. C., Lysne, P. C., Miller, C. D. and Younker, L. W., 1985, Research drilling at Inyo Domes, California: 1984 results. EOS American Geophysical Union Transactions,, Eichelberger, J. C., Lysne, P. C. and Younker, L. W., 1984, Research drilling at Inyo Domes, Long Valley Caldera, California. EOS American Geophysical Union Transactions,, Fink, J. H., Anderson, S. W. and Manley, C. R., 1992, Textural Constraints on effusive silicic volcanism: beyond the permeable foam model. Jour. Geophys. Res.,, Fink, J. H. and Manley, C. R., 1987, Origin of pumiceous and glassy textures in rhyolite flows and domes. Geol. Soc. Am. Spec. Pap.,, Hausback, B.P., 1987, An extensive, hot, vapor-charged rhyodacite flow, Baja California, Mexico. Geol. Soc. Am. Spec. Pap.,, Iddings, J. P., 1887, The nature and origin of lithophysae and the lamination of acid lavas. Am. Jour. Sci. Ser. 3., Lofgren, G., 1970, Experimental devitrification rate of rhyolite glass. Geol. Soc. Am. Bull.,,

9 Lofgren, G., 1971a, Experimentally produced devitrification textures in natural rhyolitic glass. Geol. Soc. Am. Bull.,, Lofgren, G., 1971b, Spherulite textures in glassy and crystalline rocks. Jour. Geophys. Res.,, Manley, C. R., 1992, Extended cooling and viscous flow of large, hot rhyolite lavas: implications of numerical modeling results. Jour. Volcanol. Geotherm. Res.,, Manley, C. R. and Fink, J. H., 1987,Internal textures of rhyolite flows as revealed by research drilling. Geology,, , 1991, K- Ar, 1991,., 2003, 9,, , 2004,,, Miyagi, I. and Matsubaya, O., 2003, Hydrogen isotopic composition of hornblende and biotite phenocrysts from Japanese island arc volcanoes: Evaluation of alternation process of the hydrogen isotopic ratios by degassing and re-equilibration. Jour. Volcanol. Geotherm. Res.,, Miyagi, I., Matsubaya, O. and Nakashima, S., 1998, Change in D/H ratio, water content and color during dehydration of hornblende. Geochem. Jour.,, , 1983,,, 73-82, 1985, 5 1,. Orth, K. and MacPhie, J., 2003, Texture formed during emplacement and cooling of a Palaeoproterozoic, small-volume rhyolitic sill. Jour. Volcanol. Geotherm. Res.,, Ryan, M. P. and Sammis, C. G., 1981, The glass transition in Basalt. Jour. Geophys. Res.,, Skilling, I. P., White. J. D. L. and McPhie. J., 2002, Peperite: a review of magma-sediment mingling. Jour. Volcanol. Geotherm. Res.,, Sparks, R. S. J, 1978, The dynamics of bubble formation and growth in magmas: A review and analysis. Jour. Volcanol. Geotherm. Res.,, Swanson, S. E., Naney, M. T., Westrich, H. R. and Eichelberger, J. C., 1989, Crystallization history of Obsidian Dome, Inyo Domes, California. Bull. Volcanol., Vernon, R. H., 2004, A practical guide to Rock Microstructure. The United Kingdom at the University Press, Cambridge, 594p. Vogel, T. A., Younker, L. W. and Schuraytz. B. C., 1987, Constraints on magma ascent, emplacement, and eruption: Geochemical and mineralogical data from drill-core samples at Obsidian dome, Inyo chain, California. Geology,, , 2001, 7,, 241p. Watanabe, K. and Katsui, Y., Pseudo-pillow lavas in the Aso caldera, Kyusyu, Japan. Jour. Mineral. Petrol. Econ. Geol.,, ,,, Furukawa, K. and Kamata, H., 2005, Internal Structures of the Takanoobane Rhyolite Lava in the Western Part of Aso caldera, Japan. Jour. Geol. Soc. Japan,,

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