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Page 1: Sandbox analog models:

Sandbox analog models: Sketch a cross section of the ‘mountain’ through the middle, normal to the plate boundary.Which one has higher basal coefficient of friction?

A

A’

B

B’

Page 2: Sandbox analog models:

Critical taper equation

The relationship of the topographic slope (α) to the material properties (angles of internal and basal frictions)

For cohesionless material,

𝛼=𝜇𝑏

𝑁

𝑁=𝑡𝑎𝑛2( 𝜋4 + 𝜙2 )= 1+𝑠𝑖𝑛𝜙1−𝑠𝑖𝑛𝜙

(Koons, 1990)

Page 3: Sandbox analog models:

Sandbox analog models: Construct ‘beachball ‘ diagrams showing the seismogenic instantaneous strain and fault motion.

Page 4: Sandbox analog models:

Sandbox analog models: Construct beachball diagrams.Where beachball diagrams show the predominantly strike-slip nature?

Page 5: Sandbox analog models:

Shear strain rate of weak base (φb = 15˚ ) model

Page 6: Sandbox analog models:

Shear strain rate of strong base (φb = 45˚ ) model

Page 7: Sandbox analog models:

Horizontal velocity of weak base (φb = 15˚ ) model

Page 8: Sandbox analog models:

Vertical velocity of weak base (φb = 15˚ ) model

Page 9: Sandbox analog models:

Horizontal velocity of strong base (φb = 45˚ ) model

Page 10: Sandbox analog models:

Vertical velocity of strong base (φb = 45˚ ) model


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