[CIG-SHORT] ask for help about simulation of wave field with dynamic fault

[yaoxiaodong1986]

Dear Developer,
I want to simulate the S and P wave field on the ground surface with a spontaneous rupturing dynamic fault, could you
give some advice and guidance.

The new Features in PyLith,Spatial and temporal traction variations for spontaneous rupture,does it mean that the traction restriction apply on the fault can variate spatially and temporally ,or does it meant that the simulation could compute the traction on the fault for spontaneous rupture spatially and temporally?

In PyLith Tips, Dynamic simulations Start with a static simulation. what does it mean? does it mean a simulation with dynamic fault could not start spontaneously, but start by stimulating with  kinematic fault on the rupture breaking point .

Hope for your help, thanks.

Best regards





--

祝好！
 
药晓东
 
Yao Xiaodong,  Doctor candidate 
 
College of Earth Science, Graduate University of Chinese Academy of Sciences

Address: 19A, Yuquan Road, Shijingshan City of Beijing, China

Zipcode: 100049
 
Phone:  86-10-88256339




At 2013-03-30 03:00:01,cig-short-request at geodynamics.org wrote:
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>Message: 1
>Date: Thu, 28 Mar 2013 14:46:10 -0700
>From: Brad Aagaard <baagaard at usgs.gov>
>Subject: [CIG-SHORT] LAST CALL: Your input to CIG Strategic Plan
>To: <cig-short at geodynamics.org>
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>On 03/26/2013 09:33 AM, Brad Aagaard wrote:
>> Short-Term Crustal Dynamics community:
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>> It is time to update our contribution to the CIG 5-year rolling
>> strategic plan again. I have updated the planning documents to reflect
>> discussions at our workshop last June and discussions within the PyLith
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>> adding new activities.
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>> http://www.geodynamics.org/cig/community/workinggroups/short/workarea/planning/priorities2013
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>> ACTION REQUIRED: Please submit comments by COB Thursday March 28. You
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