Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade
metamorphic processes and increasing effective stress Geology February, 2001, v. 29, p. 183-186, doi:10.1130/0091-7613(2001)029<0183:ULOTSZ>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.