[CIG-LONG] Faults do not depart away from the axis
Taichi SATO
taichix at aori.u-tokyo.ac.jp
Fri Jun 25 04:04:36 PDT 2010
Dear Walter,
I am sorry I cannot response quickly.
The new version of StrainWeakening.c works well.
However, Dike hill still remains.
I tried to fix this problem by changing the air
property and by burying the dike in the material.
I think the cause is that the dike shape cannot
move up or down with the surrounding material.
This has been mentioned by Garrett (please see the
e-mail dated April 30th, 2010).
I attached the recent input file containing air layer.
Is there any ideas to solve this problem ?
Sincerely,
Taichi
(2010/06/18 3:03), Walter Landry wrote:
> Taichi SATO<taichix at aori.u-tokyo.ac.jp> wrote:
>> Dear Garrett, Walter
>>
>>> (1) You should check the rate that the dike zone is widening. If it is
>>> widening and the fault(s) is on the side of the dike zone then the fault
>>> should be moving, except if the rate the dike is opening is about half
>>> the spreading rate (i.e., M=0.5, see Buck et al. 2005 or Behn& Ito
>>> 2008).
>> I checked the dike zone is widening(M is not 0.5).
>> So I think the fault should be depart away.
>>
>>> As a minimal hack I made the initialStrainShape be a region where the
>>> accumulated strain is always zero. It would be easy to have a maximum
>>> strain in that region as in the Buck Nature paper. I am attaching a
>>> new version of Underworld/Rheology/src/StrainWeakening.c and a
>>> modified version of the input file I sent you earlier. Right now the
>>> zero strain region is the same as the dike region. You may want to
>>> make it larger.
>>
>> I reinstalled gale after replacing with the new
>> StrainWeakening.c. I made sure that the
>> accumulated strain in the dike zone is always zero .
>> However, I also need to set initial damage to
>> weaken one side of the dike for the initiation of
>> one side fault. I think it is difficult to do this
>> by a new StrainWeakening.
>
> Here is a new version and updated input file. There is now a
> "strainLimitedShape". There is also a new parameter, "strainLimit",
> which sets the maximum strain in that shape (it defaults to zero).
>
> Cheers,
> Walter Landry
> walter at geodynamics.org
>
>
>
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