Generation of oceanic-island basalt–type volcanism in the western Trans-Mexican volcanic belt by slab rollback, asthenosphere
infiltration, and variable flux melting: Comment and Reply: COMMENT Geology September, 2002, v. 30, p. 857-858, doi:10.1130/0091-7613(2002)030<0857:GOOIBT>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.