The team’s latest work uses MEFISTO to look at the record of seismicity along the Aleutian margin. The skinny is that feedbacks between earthquake ruptures, cementation, and fluid pressure and flow account for observed clustering in the size, spacing, and timing of earthquakes!

https://pubs.geoscienceworld.org/gsa/geology/article-abstract/doi/10.1130/G48741.1/598765/How-cementation-and-fluid-flow-influence-slip

Leave a Reply

Your email address will not be published. Required fields are marked *

You may use these HTML tags and attributes:

<a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <cite> <code> <del datetime=""> <em> <i> <q cite=""> <s> <strike> <strong>