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Farallon slab detachment and deformation of the Magdalena Shelf, southern Baja California
Author(s) -
Brothers Daniel,
Harding Alistair,
GonzálezFernández Antonio,
Holbrook W. Steven,
Kent Graham,
Driscoll Neal,
Fletcher John,
Lizarralde Dan,
Umhoefer Paul,
Axen Gary
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2011gl050828
Subject(s) - geology , subduction , slab , seismology , forearc , slumping , trench , escarpment , ridge , slab window , geomorphology , paleontology , oceanic crust , tectonics , chemistry , organic chemistry , layer (electronics)
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.