New insights into the subducting oceanic crust in the Middle American Trench off western Mexico (17-19°N)

被引：16

作者：

Michaud, F

Dañobeitia, JJ

Carbonell, R

Bartolomé, R

Córdoba, D

Delgado, L

Nuñez-Cornu, F

Monfret, T

机构：

[1] Univ Paris 06, Geosci Azur, UMR 6526, F-06235 Villefranche Sur Mer, France

[2] CSIC, Inst Ciencias Tierra, Dept Geofis, E-08028 Barcelona, Spain

[3] Univ Complutense Madrid, Dept Geofis, E-28040 Madrid, Spain

[4] Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Ensenada 22830, Baja California, Mexico

[5] Univ Guadalajara, CCU Vallarta, Guadalajara 44430, Jalisco, Mexico

来源：

TECTONOPHYSICS | 2000年 / 318卷 / 1-4期

关键词：

East Pacific Rise; gravity; magnetics; Mexico; Middle America Trench; seismic reflection; subduction;

D O I：

10.1016/S0040-1951(99)00311-X

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

We present new multibeam bathymetric and multichannel seismic data on the Middle American Trench, between 17 and 19 degrees N. These data show, north of the present tip of the East Pacific Rise, unsedimented seafloor with an abyssal hill fabric bare of sediments at the outer wall of the trench (18 degrees 30'N). Two multichannel seismic profiles orthogonal to the Middle American Trench display clear oceanic crust extending more than 20 km beneath the overriding plate. These seismic images suggest that the subducting oceanic crust along the Middle American Trench is younger than previously proposed. This result, therefore, implies a new location for the East Pacific Rise termination in relation to the trench. The subduction of this young oceanic crust off western Mexico provides new constraints on the deformation and magmatism of the western Mexican mainland. (C) 2000 Elsevier Science B.V. All rights reserved.

引用

页码：187 / 200

页数：14