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Structural controls on the continent-ocean transition in the northern Gulf of California

Nagy, Elizabeth A. and Stock, Joann M. (2000) Structural controls on the continent-ocean transition in the northern Gulf of California. Journal of Geophysical Research B, 105 (B7). pp. 16251-16269. ISSN 0148-0227. https://resolver.caltech.edu/CaltechAUTHORS:20140415-125536360

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Abstract

In the Gulf of California the Pacific-North America plate boundary changes character from an oceanic-type spreading center and transform fault system (to the south) to a region of diffuse continental deformation (to the north). The presence of spreading centers commonly inferred in the northernmost gulf is not supported by bathymetric, heat flow, gravity, or seismic data which indicate significant differences north and south of latitude ∼30°N. We suggest instead that north of ∼30°N a continent-ocean transition begins which we name the Wagner Transition Zone (WTZ). Diffuse deformation characterizes the WTZ where slip occurs along reactivated north to NNW striking normal faults developed during late Miocene or Pliocene ENE directed extension. Transtensional deformation varies from ENE directed extension along dip-slip faults in the west to dextral shear along the coast to dextral-oblique slip along inferred north to NNW striking faults submerged in the northern gulf. By accounting for rotational and extensional plate motion deformation in northeastern Baja California, vector constraints require that submerged structures accommodate ∼30 mm/yr of slip in a direction slightly clockwise of the relative plate motion direction. The juxtaposition of the discrete spreading center system in the central gulf with the diffuse WTZ appears to have been a stable configuration since 4–6 Ma, perhaps controlling the evolution of spreading center jumps between Upper and Lower Tiburón and Delfin basins due to the juxtaposition of kinematically partitioned structural domains. Different histories of prerift extension and subduction-related arc magmatism along the length of the gulf, partly related to the migration of the Rivera triple junction, may explain the location of the continent-ocean transition.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/1999JB900402DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/1999JB900402/abstractPublisherArticle
ORCID:
AuthorORCID
Stock, Joann M.0000-0003-4816-7865
Additional Information:© 2000 American Geophysical Union. Manuscript Accepted: 5 Nov 1999; Manuscript Received: 12 Apr 1999. We thank Gary Axen, John Fletcher, and Associate Editor Walter Mooney for constructive thoughtful reviews which clarified the presentation of several key points. This work was supported by NSF grants EAR-9218381, EAR-9296102, and EAR-9614674, and is contribution 8620 from the Division of Geological and Planetary Sciences of the California Institute of Technology.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
NSFEAR-9218381
NSFEAR-9296102
NSFEAR-9614674
Subject Keywords:Information Related to Geographic Region: North America; Local crustal structure; Tectonophysics: Continental tectonics—extensional; Tectonophysics: Plate boundary—general
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences8620
Issue or Number:B7
Record Number:CaltechAUTHORS:20140415-125536360
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140415-125536360
Official Citation:Nagy, E. A., and J. M. Stock (2000), Structural controls on the continent-ocean transition in the northern Gulf of California, J. Geophys. Res., 105(B7), 16251–16269, doi:10.1029/1999JB900402.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:44960
Collection:CaltechAUTHORS
Deposited By: Aucoeur Ngo
Deposited On:16 Apr 2014 21:36
Last Modified:03 Oct 2019 06:24

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