Cyclic extrusion of a lava dome based on a stick-slip mechanism

被引:34
作者
Costa, A. [1 ,2 ]
Wadge, G. [2 ]
Melnik, O. [3 ]
机构
[1] Ist Nazl Geofis & Vulcanol, Naples, Italy
[2] Univ Reading, Environm Syst Sci Ctr, Reading, Berks, England
[3] Moscow MV Lomonosov State Univ, Inst Mech, Moscow, Russia
基金
俄罗斯基础研究基金会; 欧洲研究理事会;
关键词
lava dome; extrusive eruption; slip flow; periodic behaviour; dynamical system; SOUFRIERE-HILLS-VOLCANO; TEMPERATURE-DEPENDENT VISCOSITY; MOUNT ST-HELENS; WALL SLIP; MAGMA FLOW; MONTSERRAT; CONDUIT; INSTABILITIES; ERUPTIONS; DYNAMICS;
D O I
10.1016/j.epsl.2012.05.011
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Lava dome eruptions are sometimes characterised by large periodic fluctuations in extrusion rate over periods of hours that may be accompanied by Vulcanian explosions and pyroclastic flows. We consider a simple system of nonlinear equations describing a 1D flow of lava extrusion through a deep elastic dyke feeding a shallower cylindrical conduit in order to simulate this short-period cyclicity. Stick-slip conditions depending on a critical shear stress are assumed at the wall boundary of the cylindrical conduit. By analogy with the behaviour of industrial polymers in a plastic extruder, the elastic dyke acts like a barrel and the shallower cylindrical portion of the conduit as a die for the flow of magma acting as a polymer. When we applied the model to the Soufriere Hills Volcano, Montserrat, for which the key parameters have been evaluated from previous studies, cyclic extrusions with periods from 3 to 30 h were readily simulated, matching observations. The model also reproduces the reduced period of cycles observed when a major unloading event occurs due to lava dome collapse. Crown Copyright (C) 2012 Published by Elsevier B.V. All rights reserved.
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页码:39 / 46
页数:8
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