New marine geophysical data recorded across the Tonga-Kermadec subduction zone are used to image deformation and seismic velocity structures of the forearc and Pacific Plate where the Louisville Ridge seamount chain subducts. Due to the obliquity of the Louisville Ridge to the trench and the fast 128 mmyr−1 south–south west migration of the ridge-trenchcollision zone, post-,curren…

Tahun Terbit

1996

ISBN/ISSN

979-503-021-3

Deskripsi Fisik

xviii, 233p. ; ill ; 23 cm

No. Panggil

338.5 ARI t