Emplacing a Cooling-Limited Rhyolite Lava Flow: Similarities with Basaltic Lava Flows
暂无分享,去创建一个
Mike R. James | Hugh Tuffen | Charlotte Vye-Brown | M. James | C. Vye-Brown | H. Tuffen | Nathan Magnall | Nathan Magnall
[1] L. Lara,et al. Rhyodacitic fissure eruption in Southern Andes (Cordón Caulle; 40.5°S) after the 1960 (Mw:9.5) Chilean earthquake: a structural interpretation , 2004 .
[2] J. Fink. Structure and emplacement of a rhyolitic obsidian flow: Little Glass Mountain, Medicine Lake Highland, northern California , 1983 .
[3] G. Giordano,et al. Structural features of the July–August 2001 Mount Etna eruption: evidence for a complex magma supply system , 2003, Journal of the Geological Society.
[4] Christian Bignami,et al. Multisensor Satellite Monitoring of the 2011 Puyehue-Cordon Caulle Eruption , 2014, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.
[5] Harold Jeffreys M.A. D.Sc.. LXXXIV. The flow of water in an inclined channel of rectangular section , 1925 .
[6] R. C. Kerr,et al. Effect of surface solidification on the emplacement of lava flows on a slope , 2006 .
[7] S. Calvari,et al. Formation of lava tubes and extensive flow field during the 1991–1993 eruption of Mount Etna , 1998 .
[8] L. Lara,et al. High effusion rates of the Cordón Caulle 2011–2012 eruption (Southern Andes) and their relation with the quasi‐harmonic tremor , 2015 .
[9] O. Merle,et al. Extensional and compressional strain in lava flows and the formation of fractures in surface crust , 2005 .
[10] Murphy,et al. Control on the emplacement of the andesite lava dome of the Soufriere Hills volcano, Montserrat by degassing‐induced crystallization , 2000 .
[11] S. Anderson,et al. Mount St. Helens and Santiaguito lava domes: The effect of short-term eruption rate on surface texture and degassing processes , 1995 .
[12] H. Mader,et al. The rheology of two-phase magmas: A review and analysis , 2013 .
[13] John R. Lister,et al. Viscous flows down an inclined plane from point and line sources , 1992, Journal of Fluid Mechanics.
[14] M. James,et al. Examining rhyolite lava flow dynamics through photo-based 3D reconstructions of the 2011–2012 lava flowfield at Cordón-Caulle, Chile , 2014 .
[15] S. Calvari,et al. Morphological complexities and hazards during the emplacement of channel-fed `a`ā lava flow fields: A study of the 2001 lower flow field on Etna , 2010 .
[16] C. Kilburn. Fracturing as a quantitative indicator of lava flow dynamics , 2004 .
[17] J. Fink. Surface folding and viscosity of rhyolite flows , 1980 .
[18] A. Harris,et al. The thermal stealth flows of Santiaguito dome, Guatemala: Implications for the cooling and emplacement of dacitic block-lava flows , 2002 .
[19] H. Morenoa,et al. Rhyodacitic fissure eruption in Southern Andes ( Cordón Caulle ; 40 . 5 8 S ) after the 1960 ( Mw : 9 . 5 ) Chilean earthquake : a structural interpretation , 2004 .
[20] J. Fink,et al. Hydrogen isotope analysis of rehydrated silicic lavas: implications for eruption mechanisms , 2001 .
[21] C. R. Manley. Extended cooling and viscous flow of large, hot rhyolite lavas: implications of numerical modeling results , 1992 .
[22] Boris Behncke,et al. The July–August 2001 eruption of Mt. Etna (Sicily) , 2003 .
[23] Lionel Wilson,et al. Factors controlling the lengths of channel-fed lava flows , 1994 .
[24] A. Harris,et al. The evolution of an active silicic lava flow field: an ETM+ perspective , 2004 .
[25] John R. Stephenson,et al. Introduction to special section : Long lava flows. , 1998 .
[26] P. Whelley,et al. Rhyolite lava dome growth styles at Chaitén Volcano, Chile (2008-2009): Interpretation of thermal imagery , 2013 .
[27] C. Bonadonna,et al. Complex dynamics of small-moderate volcanic events: the example of the 2011 rhyolitic Cordón Caulle eruption, Chile , 2015, Bulletin of Volcanology.
[28] S. Blake,et al. Modelling the emplacement of compound lava flows , 2000 .
[29] T. Barry,et al. Architecture and emplacement of flood basalt flow fields: case studies from the Columbia River Basalt Group, NW USA , 2013, Bulletin of Volcanology.
[30] R. W. Griffiths,et al. Morphology, eruption rates, and rheology of lava domes - Insights from laboratory models , 1998 .
[31] J. Lowenstern,et al. The Chaitén rhyolite lava dome: Eruption sequence, lava dome volumes, rapid effusion rates and source of the rhyolite magma , 2013 .
[32] D. Dingwell,et al. Viscosity of magmatic liquids: A model , 2008 .
[33] J. Fink,et al. Internal textures of rhyolite flows as revealed by research drilling , 1987 .
[34] O. Melnik,et al. Eruption mechanisms and short duration of large rhyolitic lava flows of Yellowstone , 2017 .
[35] A. Amigo,et al. Storage and eruption of near-liquidus rhyolite magma at Cordón Caulle, Chile , 2013, Bulletin of Volcanology.
[36] M. T. Naney,et al. Crystallization history of Obsidian Dome, Inyo Domes, California , 1989 .
[37] A. Whittington,et al. Thermal diffusivity of rhyolitic glasses and melts: effects of temperature, crystals and dissolved water , 2012, Bulletin of Volcanology.
[38] G. Walker. Compound and simple lava flows and flood basalts , 1971 .
[39] A. Rust,et al. Evolution of crust- and core-dominated lava flows using scaling analysis , 2013, Bulletin of Volcanology.
[40] Eugenio Rustico,et al. Numerical simulation of lava flow using a GPU SPH model , 2011 .
[41] N. Bridges. Ambient effects on basalt and rhyolite lavas under Venusian, subaerial, and subaqueous conditions , 1997 .
[42] Daniele Andronico,et al. Analysis of the 2001 lava flow eruption of Mt. Etna from three-dimensional mapping , 2007 .
[43] Ciro Del Negro,et al. Modeling of the 2001 lava flow at Etna volcano by a Cellular Automata approach , 2007, Environ. Model. Softw..
[44] R. C. Kerr,et al. Effects of internal rheology and surface cooling on the emplacement of lava flows , 2005 .
[45] L. Lara,et al. Magmatic evolution of the Puyehue–Cordón Caulle Volcanic Complex (40° S), Southern Andean Volcanic Zone: From shield to unusual rhyolitic fissure volcanism , 2006 .
[46] J. Kauahikaua,et al. The transition from 'A'ā to Pāhoehoe crust on flows emplaced during the Pu'u 'ō'Ō-Kupaianaha eruption , 2003 .
[47] K. Cashman,et al. Constraints on rheology of obsidian lavas based on mesoscopic folds , 1999 .
[48] G. Hulme,et al. The Interpretation of Lava Flow Morphology , 1974 .
[49] M. James,et al. Exceptional mobility of an advancing rhyolitic obsidian flow at Cordón Caulle volcano in Chile , 2013, Nature Communications.
[50] Sonia Calvari,et al. Multidisciplinary approach yields insight into Mt. Etna eruption , 2001 .
[51] S. Anderson,et al. Pulsed inflation of pahoehoe lava flows: implications for flood basalt emplacement , 1999 .
[52] G. M. Crisci,et al. Lava Flow Simulation Bv A Discrete Cellular Model: First Implementation , 1986 .
[53] J. Fink. Gravity instability in the Holocene Big and Little Glass Mountain rhyolitic obsidian flows, northern California , 1980 .
[54] S. Anderson,et al. Crease structures: Indicators of emplacement rates and surface stress regimes of lava flows , 1992 .
[55] Benoit Cordonnier,et al. Rapid laccolith intrusion driven by explosive volcanic eruption , 2016, Nature Communications.
[56] Michael P. Poland,et al. Tracking lava flow emplacement on the east rift zone of Kīlauea, Hawai‘i, with synthetic aperture radar coherence , 2012 .
[57] A. Pantoja,et al. Cristobalite in the 2011–2012 Cordón Caulle eruption (Chile) , 2015, Bulletin of Volcanology.
[58] Martin O. Saar,et al. Numerical models of the onset of yield strength in crystal–melt suspensions , 2001 .
[59] Jonathan H. Fink,et al. Effects of surface cooling on the spreading of lava flows and domes , 1993, Journal of Fluid Mechanics.
[60] M. James,et al. Shallow vent architecture during hybrid explosive–effusive activity at Cordón Caulle (Chile, 2011–12): Evidence from direct observations and pyroclast textures , 2013 .
[61] Herbert E. Huppert,et al. Flow and instability of a viscous current down a slope , 1982, Nature.
[62] L. Applegarth. Complexity in Lava Flows: Surface Features and Structural Morphology , 2008 .
[63] L. Lara,et al. The 2011-2012 eruption of Cordón Caulle volcano (Southern Andes): Evolution, crisis management and current hazards , 2012 .
[64] K. Cashman,et al. Structural origin of large gas cavities in the Big Obsidian Flow, Newberry Volcano , 2002 .
[65] J. P. Kauahikaua,et al. Emplacement and inflation of pahoehoe sheet flows: observations and measurements of active lava flows on Kilauea volcano, Hawaii , 1994 .
[66] J. Phillips,et al. Degassing processes during lava dome growth: Insights from Santiaguito lava dome, Guatemala , 2011 .
[67] H. Westrich,et al. Non-explosive silicic volcanism , 1986, Nature.
[68] S. Anderson,et al. Textural constraints on effusive silicic volcanism - Beyond the permeable foam model , 1992 .
[69] J. Eichelberger. Silicic Volcanism: Ascent of Viscous Magmas from Crustal Reservoirs , 1995 .
[70] Alison C Rust,et al. Rheology and flow of crystal-bearing lavas: Insights from analogue gravity currents , 2010 .
[71] H. C. Heard,et al. Thermal diffusivity of igneous rocks at elevated pressure and temperature , 1987 .
[72] Y. Katsui,et al. Lateral Fissure Eruptions in the Southern Andes of Chile , 1967 .
[73] D. Dingwell,et al. Measurement and implication of "effective" viscosity for rhyolite flow emplacement , 2001 .
[74] W. Rose. Santa María, Guatemala: Bimodal soda-rich calc-alkalic stratovolcano , 1987 .
[75] H. Mader,et al. The effect of particle shape on suspension viscosity and implications for magmatic flows , 2011 .
[76] E. Fujita,et al. VTFS project: Development of the lava flow simulation code LavaSIM with a model for three‐dimensional convection, spreading, and solidification , 2005 .
[77] S. Blake. Viscoplastic Models of Lava Domes , 1990 .
[78] R. C. Kerr,et al. Importance of surface crust strength during the flow of the 1988–1990 andesite lava of Lonquimay Volcano, Chile , 2007 .
[79] T. Grove,et al. The evolution of young silicic lavas at Medicine Lake Volcano, California: Implications for the origin of compositional gaps in calc-alkaline series lavas , 1986 .