FACW_GEOL_2012_19448007_Brothers_Harding_GonzálezFernández_Holbrook_Kent_Driscoll_Fletcher_Lizarralde_Umhoefer_Axen.pdf (6.04 MB)
Farallon Slab Detachment and Deformation of the Magdalena Shelf, Southern Baja California
journal contribution
posted on 2021-11-15, 21:36 authored by Daniel Brothers, Alistair Harding, Antonio González-Fernández, W. Steven Holbrook, Graham Kent, Neal Driscoll, John Fletcher, Dan Lizarralde, Paul Umhoefer, Gary AxenSubduction 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 (~24.5N) 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.
History
ISO
engLanguage
EnglishPublisher
University of Wyoming. LibrariesJournal title
Geophysical Research LettersCollection
Faculty Publication - Geology & GeophysicsDepartment
- Library Sciences - LIBS