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Caldera geometry determined by the depth of the magma chamber
Earth, Planets and Space volume 57, pagese17–e20(2005)
The depth of the magma chamber is shown to be an important factor governing the initial type, scale, and collapse of a caldera. The collapse of the magma chamber is approximated by the contraction of a sphere in an elastic medium, and the distribution of plastic and/or rupturing area on the surface is calculated using the Coulomb failure criterion under the assumption of an elastic-perfectly plastic material. It is found that the necessary contraction for the formation of a caldera is described by fifth-power polynomial expression of the depth of the magma chamber, and that the radius and geometry of the caldera are dependent on the depth of the magma chamber.
Acocella, V., F. Cifelli and R. Funiciello, Analogue models of collapse calderas and resurgent domes, J. Volcanol. Geotherm. Res., 104, 81–96, 2000.
Gudmundsson, A., Effect of tensile stress concentration around magma chambers on intrusion and extrusion frequencies, J. Volcanol. Geotherm. Res., 35, 179–194, 1988.
Gudmundsson, A., Formation and development of normal-fault calderas and the initiation of large explosive eruptions, Bull. Volcanol., 60, 160–170, 1998.
Gudmundsson, A., Emplacement and arrest of sheets and dykes in central volcanoes, J. Volcanol. Geotherm. Res., 116, 279–298, 2002.
Gudmundsson, A., Surface stresses associated with arrested dykes in rift zones, Bull. Volcanol., 65, 606–619, 2003.
Gudmundsson, A., J. Marti, and E. Turon, Stress fields generating ring faults in volcanoes, Geophys. Res. Lett., 24, 1559–1562, 1997.
Hagiwara, Y., Theory of Geogravity, Kyoritsu-zensyo, Tokyo, 242 pp., 1978 (in Japanese).
Jaeger, J. C. and N. G. Cook, Fundamentals of Rock Mechanics, Methuen, London, 513 pp., 1969.
Komuro, H., Experiments on cauldron formation: a polygonal cauldron and ring fractures, J. Volcanol. Geotherm. Res., 31, 139–149, 1987.
Kusumoto, S. and K. Takemura, Numerical simulation of caldera formation due to collapse of a magma chamber, Geophys. Res. Lett., 30(24), 2278, doi10.1029/2003GL018380, 2003.
Lipman, P. W., Subsidence of ash-flow calderas: relation to caldera size and magma-chamber geometry, Bull. Volcanol., 59, 198–218, 1997.
Marti, J., G. J. Ablay, L. T. Redshaw, and R. S. J. Sparks, Experimental studies of collapse calderas, J. Geol. Soc. London, 151, 919–929, 1994.
McTigue, D. F., Elastic stress and deformation near a finite spherical magma body: resolution of the point source paradox, J. Geophys. Res., 92, 12931–12940, 1987.
Mogi, K., Relations between eruptions of various volcanoes and the deformation of the ground surface around them, Bull. Earthquake Res. Inst., 36, 99–134, 1958.
Nakamura, K., Volcanoes as possible indicators of tectonic stress orientation—principle and proposal, J. Volocanol. Geotherm. Res., 2, 1–16, 1977.
Roche, O., T. H. Druitt, and O. Merle, Experimental study of caldera formation, J. Geophys. Res., 105, 395–416, 2000.
Rymer, H., B. van Vries, J. Stix, and G. Williams-Jones, Pit crater structure and processes governing persistent activity at Masaya volcano, Nicaragua, Bull. Volcanol., 59, 345–355, 1998.
Segall. P. and D. D. Pollard, Mechanics of Discontinuous Faults, J. Geophys. Res., 85, 4337–4350, 1980.
Tsuchida, E. and I. Nakahara, Stresses in a semi-infinite body subjected to uniform pressure on the surface of a cavity and the plane boundary, Bull. JSME, 15, 1–12, 1972.
Yamaji, A., Introduction to Theoretical Tectonics, Asakura Syoten, Tokyo, 287 pp., 2000 (in Japanese).
Yoshida, T., Tertiary Ishizuki cauldron, southwestern Japan arc formation by ring fracture subsidence, J. Geophys. Res., 89, 8502–8510, 1984.
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Kusumoto, S., Takemura, K. Caldera geometry determined by the depth of the magma chamber. Earth Planet Sp 57, e17–e20 (2005). https://doi.org/10.1186/BF03351879
- magma chamber
- caldera geometry
- depth of magma chamber
- numerical simulation