title: Seismology: tectonic strain in plate interiors?
abstract: It is not fully understood how or why the inner areas of tectonic plates deform, leading to large, although infrequent, earthquakes. Smalley et al. offer a potential breakthrough by suggesting that surface deformation in the central United States accumulates at rates comparable to those across plate boundaries. However, we find no statistically significant deformation in three independent analyses of the data set used by Smalley et al., and conclude therefore that only the upper bounds of magnitude and repeat time for large earthquakes can be inferred at present.
authors.affiliation: Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907, USA. ecalais@purdue.edu
authors.forename: E
authors.initials: E
authors.lastname: Calais
authors.forename: G
authors.initials: G
authors.lastname: Mattioli
authors.forename: C
authors.initials: C
authors.lastname: DeMets
authors.forename: J-M
authors.initials: JM
authors.lastname: Nocquet
authors.forename: S
authors.initials: S
authors.lastname: Stein
authors.forename: A
authors.initials: A
authors.lastname: Newman
authors.forename: P
authors.initials: P
authors.lastname: Rydelek