Buoyancy-driven fluid fracture: similarity solutions for the horizontal and vertical propagation of fluid-filled cracks
暂无分享,去创建一个
[1] J. Weertman. Theory of water-filled crevasses in glaciers applied to vertical magma transport beneath oceanic ridges , 1971 .
[2] D. Pollard,et al. On the mechanical interaction between a fluid-filled fracture and the earth's surface , 1979 .
[3] N. Muskhelishvili. Some basic problems of the mathematical theory of elasticity , 1953 .
[4] H. Huppert,et al. Cooling and contamination of mafic and ultramafic magmas during ascent through continental crust , 1985 .
[5] John R. Lister,et al. Buoyancy-driven fluid fracture: the effects of material toughness and of low-viscosity precursors , 1990, Journal of Fluid Mechanics.
[6] E. D. Jackson,et al. Orientation and growth of Hawaiian volcanic rifts: the effect of regional structure and gravitational stresses , 1972, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.
[7] D. Swanson,et al. Linear vent systems and estimated rates of magma production and eruption for the Yakima Basalt on the Columbia Plateau , 1975 .
[8] R. C. Kerr,et al. Fluid‐mechanical models of crack propagation and their application to magma transport in dykes , 1991 .
[9] Josefino C. Comiso,et al. Characteristics of Arctic winter sea ice from satellite multispectral microwave observations , 1986 .
[10] H. Huppert. The propagation of two-dimensional and axisymmetric viscous gravity currents over a rigid horizontal surface , 1982, Journal of Fluid Mechanics.
[11] J. Fink,et al. The mechanism of intrusion of the Inyo Dike, Long Valley Caldera, California , 1988 .
[12] R. C. Kerr,et al. The propagation of two-dimensional and axisymmetric viscous gravity currents at a fluid interface , 1989, Journal of Fluid Mechanics.
[13] H. Huppert,et al. Emplacement and cooling of komatiite lavas , 1984, Nature.
[14] Herbert E. Huppert,et al. Flow and instability of a viscous current down a slope , 1982, Nature.
[15] G. Walker. Gravitational (density) controls on volcanism, magma chambers and intrusions , 1989 .
[16] R. Macdonald,et al. Emplacement of the Cleveland Dyke: Evidence from Geochemistry, Mineralogy, and Physical Modelling , 1988 .
[17] S. Maaløe. The generation and shape of feeder dykes from mantle sources , 1987 .
[18] P. W. Sharp,et al. Self-similar solutions for elastohydrodynamic cavity flow , 1985, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.
[19] Keiiti Aki,et al. Source mechanism of volcanic tremor: fluid-driven crack models and their application to the 1963 kilauea eruption , 1977 .
[20] D. Turcotte,et al. Buoyancy‐driven magma fracture: A mechanism for ascent through the lithosphere and the emplacement of diamonds , 1990 .
[21] J. Pasteris. KIMBERLITES: COMPLEX MANTLE MELTS , 1984 .
[22] D. Pollard,et al. The effect of gradients in regional stress and magma pressure on the form of sheet intrusions in cross section , 1976 .
[23] P. C. Grew,et al. Stress corrosion theory of crack propagation with applications to geophysics , 1977 .
[24] Peter C. Smith,et al. A similarity solution for slow viscous flow down an inclined plane , 1973, Journal of Fluid Mechanics.
[25] G. G. Hirs. A Systematic Study of Turbulent Film Flow , 1974 .
[26] J. Nicholls,et al. High-temperature properties of silicate liquids: applications to the equilibration and ascent of basic magma , 1977, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[27] H. Huppert,et al. Thermal control of basaltic fissure eruptions , 1989, Nature.