Rapid subsidence and sedimentation from oblique slip near a bend on the North Anatolian transform fault in the Marmara Sea,
Turkey Geology November, 2006, v. 34, p. 933-936, doi:10.1130/G22520A.1
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.