The role of off-fault damage in the evolution of normal faults

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

13

Fault Slip Profiles, Damage, Afar Normal Faults

Scientific paper

Recent measurements of slip profiles on normal faults have found that they are usually triangular in shape. This has been explained to be a consequence of on-fault processes such as slip-dependent friction. However, the recent observation that cumulative slip profiles on normal faults and fault systems in Afar are both triangular and self-similar excludes this explanation and requires some form of off-fault deformation. Here, we use elastic modelling to show that large triangular zones of off-fault damage can explain the observed triangular slip profiles provided damage is anisotropic in the form of cracks sub-parallel to the fault. Our modelling suggests that these triangular damage zones result from the enlargement of the crack tip damage area as the fault (or system) lengthens. Our modelling also demonstrates that different types of `barriers' can cause the slip profiles to terminate abruptly at one or both fault ends, as observed in Afar and elsewhere.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

The role of off-fault damage in the evolution of normal faults does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with The role of off-fault damage in the evolution of normal faults, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The role of off-fault damage in the evolution of normal faults will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1549614

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.