Skip to main content

Currently Skimming:

Geometric incompatibility in a fault system
Pages 3838-3842

The Chapter Skim interface presents what we've algorithmically identified as the most significant single chunk of text within every page in the chapter.
Select key terms on the right to highlight them within pages of the chapter.


From page 3838...
... 1 act as transient asperities, and unlocked junctions may act as transient weakest links. Tentative estimates of K and G are made for each end of the Big Bend of the San Andreas fault system in Southern California.
From page 3839...
... 2~. Geometric Incompatibility for a System of Faults with Multiple Junctions We consider here the case of rigid nonrotating blocks, which is analytically simpler than the general case and can be of independent interest.
From page 3840...
... the value G for the region D equals the sum of the values G for all fault junctions that exist inside D at the time moment to. Application to Southern California Fault Junctions To illustrate the method suggested here, we considered a schematic representation of two nodes with multiple fault junctions around the ends of the Big Bend segment of the San Andreas fault.
From page 3841...
... In particular, it may be one of the parameters that controls the dynamics of seismicity. Appendix: Incompatibilities for Deformable and Rotating Blocks For a system of deformable blocks, the Saint Venant compatibility condition, in the integral form, can be written as follows (ref.
From page 3842...
... Army Research Office through the Mathematical Sciences Institute of Cornell University, Contract DAAL03-91-C-0027, and Department of Geological Sciences at Cornell University, under National Science Foundation Grant no.


This material may be derived from roughly machine-read images, and so is provided only to facilitate research.
More information on Chapter Skim is available.