Holocene slip rates along the Owens Valley fault, California: Implications for the recent evolution of the Eastern California
Shear Zone Geology September, 2001, v. 29, p. 819-822, doi:10.1130/0091-7613(2001)029<0819:HSRATO>2.0.CO;2
To use Bloc of Docs to access this article, or to purchase additional credits, you must first sign in above with your personal
user name and password.
If you do not have a login you may activate a subscription or register
to obtain a user name and password for free.