Farallon slab detachment and deformation of the Magdalena Shelf, southern Baja California
Geophysical Research Letters
By: Daniel S. Brothers, Alistair J. Harding, Antonio Gonzalez-Fernandez, W.S. Steven Holbrook, Graham M. Kent, Neal W. Driscoll, John M. Fletcher, Daniel Lizarralde, Paul J. Umhoefer, and Gary Axen
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Abstract
Subduction of the Farallon plate beneath northwestern Mexico stalled by ~12 Ma when the Pacific-Farallon spreading-ridge approached the subduction zone. Coupling between remnant slab and the overriding North American plate played an important role in the capture of the Baja California (BC) microplate by the Pacific Plate. Active-source seismic reflection and wide-angle seismic refraction profiles across southwestern BC (~24.5°N) are used to image the extent of remnant slab and study its impact on the overriding plate. We infer that the hot, buoyant slab detached ~40 km landward of the fossil trench. Isostatic rebound following slab detachment uplifted the margin and exposed the Magdalena Shelf to wave-base erosion. Subsequent cooling, subsidence and transtensional opening along the shelf (starting ~8 Ma) starved the fossil trench of terrigenous sediment input. Slab detachment and the resultant rebound of the margin provide a mechanism for rapid uplift and exhumation of forearc subduction complexes.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Farallon slab detachment and deformation of the Magdalena Shelf, southern Baja California |
| Series title | Geophysical Research Letters |
| DOI | 10.1029/2011GL050828 |
| Volume | 39 |
| Issue | 9 |
| Year Published | 2012 |
| Language | English |
| Publisher | Wiley |
| Contributing office(s) | Woods Hole Coastal and Marine Science Center |
| Description | L09307 |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Geophysical Research Letters |
| Country | Mexico |
| State | Baja California |
| Google Analytic Metrics | Metrics page |