Seismic structure of the southern Gulf of California from Los Cabos block to the East Pacific Rise

P. Páramo, W. S. Holbrook, H. E. Brown, D. Lizarralde, J. Fletcher, Paul J Umhoefer, G. Kent, A. Harding, A. Gonzalez, G. Axen

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Multichannel reflection and coincident wide-angle seismic data collected during the 2002 Premier Experiment, Sea of Cortez, Addressing the Development of Oblique Rifting (PESCADOR) experiment provide the most detailed seismic structure to date of the southern Gulf of California. Multichannel seismic (MCS) data were recorded with a 6-km-long streamer, 480-channel, aboard, the R/V Maurice Ewing, and wide-angle data was recorded by 19 instruments spaced every ∼12 km along the transect. The MCS and wide-angle data reveal the seismic structure across the continent-ocean transition of the rifted margin. Typical continental and oceanic crust are separated by a ∼75-km-wide zone of extended continental crust dominated by block-faulted basement. Little lateral variation in crustal thicknesses and seismic velocities is observed in the oceanic crust, suggesting a constant rate of magmatic productivity since seafloor spreading began. Oceanic crustal thickness and mean crustal velocities suggest normal mantle temperature (1300°C) and passive mantle upwelling at the early stages of seafloor spreading. The crustal thickness, width of extended continental crust, and predicted temperature conditions all indicate a narrow rift mode of extepsion. On the basis of upper and lower crust stretching factors, an excess of lower crust was found in the extended continental crust. Total extension along transect 5W is estimated to be ∼35 km. Following crustal extension, new oceanic crust ∼6.4-km-thick was formed at a rate of ∼48 mm a-1 to accommodate plate separation.

Original languageEnglish (US)
Article numberB03307
JournalJournal of Geophysical Research E: Planets
Volume113
Issue number3
DOIs
StatePublished - Mar 4 2008

Fingerprint

Gulf of California (Mexico)
Gulf of California
continental crust
crusts
crustal thickness
oceanic crust
seafloor spreading
lower crust
Stretching
seismic data
transect
Productivity
Experiments
ocean-continent transition
Temperature
temperature
seismic velocity
oceans
upper crust
rifting

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Atmospheric Science
  • Astronomy and Astrophysics
  • Oceanography

Cite this

Seismic structure of the southern Gulf of California from Los Cabos block to the East Pacific Rise. / Páramo, P.; Holbrook, W. S.; Brown, H. E.; Lizarralde, D.; Fletcher, J.; Umhoefer, Paul J; Kent, G.; Harding, A.; Gonzalez, A.; Axen, G.

In: Journal of Geophysical Research E: Planets, Vol. 113, No. 3, B03307, 04.03.2008.

Research output: Contribution to journalArticle

Páramo, P, Holbrook, WS, Brown, HE, Lizarralde, D, Fletcher, J, Umhoefer, PJ, Kent, G, Harding, A, Gonzalez, A & Axen, G 2008, 'Seismic structure of the southern Gulf of California from Los Cabos block to the East Pacific Rise', Journal of Geophysical Research E: Planets, vol. 113, no. 3, B03307. https://doi.org/10.1029/2007JB005113
Páramo, P. ; Holbrook, W. S. ; Brown, H. E. ; Lizarralde, D. ; Fletcher, J. ; Umhoefer, Paul J ; Kent, G. ; Harding, A. ; Gonzalez, A. ; Axen, G. / Seismic structure of the southern Gulf of California from Los Cabos block to the East Pacific Rise. In: Journal of Geophysical Research E: Planets. 2008 ; Vol. 113, No. 3.
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