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GPFW04 |
17th September 2003
09:15 to 09:20 |
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Introduction |
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GPFW04 |
17th September 2003
09:20 to 10:20 |
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Laboratory constraints on hydromechanical weakening of granular fault gouge during earthquake slip |
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GPFW04 |
17th September 2003
10:20 to 11:00 |
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Effects of shear heating on stability of a dilatant, fluid-saturated fault zone |
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GPFW04 |
17th September 2003
11:30 to 12:00 |
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Heating, weakening and partial melting of rapidly sheared fault gouge |
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GPFW04 |
17th September 2003
12:00 to 12:30 |
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Field examples of liquefaction, mudslides and rock avalanches, and problems as to mechanisms |
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GPFW04 |
17th September 2003
13:40 to 14:20 |
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Fluidisation in artesian flow conditions: cases of hydromechanically stable versus unstable granular media |
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GPFW04 |
17th September 2003
14:20 to 15:00 |
AC Palmer |
Wave-induced liquefaction of the seabed around submarine pipelines |
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GPFW04 |
17th September 2003
15:30 to 16:10 |
RM Iverson |
Dilatancy and pore-pressure feedback as causes of diverse styles and rates of landslide motion |
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GPFW04 |
17th September 2003
16:10 to 16:50 |
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Mud/lava viscoplastic flow downslope |
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GPFW04 |
17th September 2003
16:50 to 17:20 |
K Hutter |
Avalanches of snow, debris and mud - geophysical systems between order and disorder |
