Abstract

The postearthquake deformation of a geodetic network which spans the zone of rupture of the 1966 Parkfield earthquake is not pure right-lateral shear as might be expected but rather is primarily an east-west extension. This deformation is consistent with that predicted by a dilatancy model.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.