Three fragmentation mechanisms for highly viscous magma under rapid decompression

[1]  D. Dingwell.  The Brittle-Ductile Transition in High-Level Granitic Magmas: Material Constraints , 1997 .

[2]  R. Stevenson,et al.  Physical properties of the 1980 Mount St. Helens cryptodome magma , 1997 .

[3]  B. Sturtevant,et al.  Dynamics of gas‐driven eruptions: Experimental simulations using CO2‐H2O‐polymer system , 1997 .

[4]  M. Alidibirov,et al.  An experimental facility for the investigation of magma fragmentation by rapid decompression , 1996 .

[5]  K. Cashman,et al.  Permeability development in vesiculating magmas: implications for fragmentation , 1996 .

[6]  M. Alidibirov,et al.  Magma fragmentation by rapid decompression , 1996, Nature.

[7]  B. Sturtevant,et al.  Dynamics of explosive degassing of magma: Observations of fragmenting two-phase flows , 1996 .

[8]  J. Phillips,et al.  Gum rosin-acetone system as an analogue to the degassing behaviour of hydrated magmas , 1995 .

[9]  M. Bursik,et al.  Explosive fragmentation of erupting magma , 1995, Nature.

[10]  D. Dingwell.  Relaxation in silicate melts; some applications , 1995 .

[11]  M. Alidibirov,et al.  A model for viscous magma fragmentation during volcanic blasts , 1994 .

[12]  B. Sturtevant,et al.  Experimental simulations of explosive degassing of magma , 1994, Nature.

[13]  R. Harmon,et al.  Bimodal Density Distribution of Cryptodome Dacite from the 1980 Eruption of Mount St. Helens, Washington , 1993 .

[14]  S. Kieffer,et al.  Estimate of pyroclastic flow velocities resulting from explosive decompression of lava domes , 1993, Nature.

[15]  B. Sturtevant,et al.  Geological implications and applications of high-velocity two-phase flow experiments , 1993 .

[16]  S. Nakada,et al.  Crumbling of dacite dome lava and generation of pyroclastic flows at Unzen volcano , 1992, Nature.

[17]  J. Litwiniszyn.  Remarks on the equations of state of outburst rocks regarded as a solid solution , 1991 .

[18]  Gary A. Smith,et al.  Sedimentation in Volcanic Settings , 1991 .

[19]  D. Dingwell,et al.  Non-Newtonian Rheology of Igneous Melts at High Stresses and Strain Rates: Experimental Results for Rhyolite, Andesite, Basalt, and Nephelinite , 1990 .

[20]  D. Dingwell,et al.  Structural relaxation in silicate melts and non-Newtonian melt rheology in geologic processes , 1989 .

[21]  K. Cashman.  Crystallization of Mount St. Helens 1980–1986 dacite: A quantitative textural approach , 1988 .

[22]  M. E. Kipp,et al.  10 – DYNAMIC ROCK FRAGMENTATION , 1987 .

[23]  B. Atkinson.  Fracture Mechanics of Rock , 1987 .

[24]  R. Sparks,et al.  The initial giant umbrella cloud of the May 18th, 1980, explosive eruption of Mount St. Helens , 1986 .

[25]  Tsutomu Murase,et al.  Viscosity of the dome of mount St. Helens , 1985 .

[26]  J. Eichelberger,et al.  Magmatic model for the Mount St. Helens blast of May 18, 1980 , 1982 .

[27]  S. Self,et al.  Vulcanian eruption mechanisms , 1979, Nature.

[28]  G. Heiken.  Plinian-type eruptions in the medicine lake highland, california, and the nature of the underlying magma , 1978 .

[29]  R. Sparks,et al.  The dynamics of bubble formation and growth in magmas , 1978 .

[30]  W. Rose,et al.  Nuée ardente eruption from the foot of a dacite lava flow, Santiaguito volcano, Guatemala , 1976 .

[31]  A. McBirney,et al.  Factors governing the formation of pyroclastic rocks , 1970 .

[32]  J. Verhoogen.  Mechanics of ash formation , 1951 .