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Pliocene–Quaternary subsidence and exhumation of the southeastern San Joaquin Basin, California, in response to mantle lithosphere removal

Cecil, M. Robinson and Saleeby, Z. and Saleeby, J. and Farley, K. A. (2014) Pliocene–Quaternary subsidence and exhumation of the southeastern San Joaquin Basin, California, in response to mantle lithosphere removal. Geosphere, 10 (1). pp. 129-147. ISSN 1553-040X. https://resolver.caltech.edu/CaltechAUTHORS:20140805-103825342

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Abstract

Thermomechanical models of mantle lithosphere removal from beneath the southern Sierra Nevada region, California (USA), predict a complex spatiotemporal pattern of vertical surface displacements. We evaluate these models by using (U-Th)/He thermochronometry, together with other paleothermometry estimates, to investigate such topographic transients. We target Tertiary strata from the Kern arch, a crescent-shaped active uplift located in the southeastern San Joaquin Basin, along the western flank of the southern Sierra Nevada. Kern arch stratigraphy provides a unique record of subsidence and exhumation in a sensitive region immediately adjacent to the delaminating mantle lithosphere at depth. Detrital apatite (U-Th)/He ages from Oligocene–Miocene sandstones collected in Kern arch well cores indicate postdepositional heating to temperatures beyond those corresponding with their present burial depths. When integrated with available geologic and stratigraphic constraints, temperature-time modeling of thermochronometric data suggests partial He loss from apatites at temperatures of 70–90 °C, followed by exhumation to present burial temperatures of 35–60 °C since ca. 6 Ma. By constraining the late Cenozoic geothermal gradient to ∼25 °C/km, our results imply 1.0–1.6 km of rapid (∼0.4 mm/yr) subsidence and sedimentation, and then subsequent uplift and exhumation of southeastern San Joaquin Basin strata in latest Miocene–Quaternary time. Stratigraphic and geomorphic relations further constrain the principal burial episode to ca. 2.5 Ma or later, and exhumation to ca. 1 Ma or later. Subtle differences in the maximum temperatures achieved in various wells may reflect differing degrees of tectonic subsidence and sedimentation as a function of growth faulting and distance from the range front. Our results are consistent with estimates of surface subsidence and uplift from Sierran delamination models, which predict a minimum of ∼0.7 km of tectonic subsidence in regions retaining mantle lithosphere adjacent to the area of delamination, and a minimum of ∼0.8 km of rock uplift in regions where delamination occurred recently. We attribute the marked pulse of tectonic subsidence in the San Joaquin Basin to viscous coupling between the lower crust and a downwelling mass in the delaminating slab. The ensuing episode of exhumation is interpreted to result from the northwestward peeling back of the slab and the associated replacement of dense lithosphere with buoyant asthenosphere that drove rapid rock and surface uplift.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1130/GES00882.1DOIArticle
http://geosphere.gsapubs.org/content/10/1/129.abstractPublisherArticle
http://geosphere.geoscienceworld.org/content/10/1/129PublisherArticle
http://geosphere.geoscienceworld.org/content/10/1/129/suppl/DC1PublisherSupplemental File
Additional Information:© 2014 Geological Society of America. Received 24 January 2013; Revision received 13 September 2013; Accepted 16 December 2013; Published online 14 January 2014. We thank S.A. Reid, J.R. Boles, M. Irskine, Eric Hierling, and the California State University, Bakersfi eld, California Well Sample Repository (CWSR) for assistance in securing core samples. Joerg Mattner provided sidewall core from the Smoot well, as well as useful discussion about the Kern arch. We benefi ted greatly from laboratory assistance by Alan Chapman and Lindsey Hedges and from conversations with Laetitia Le Pourhiet, Jan Gillspie, S.A. Graham, and D.D. Miller. An early version of this manuscript benefi ted from the critical reviews of Mark Brandon, Craig Jones, and Rob Negrini. This work was supported by National Science Foundation grant EAR-0606903 to J. Saleeby, and by a grant from the Gordon and Betty Moore Foundation. This is contribution 208 of the Tectonics Observatory at the California Institute of Technology.
Group:Caltech Tectonics Observatory
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Funding AgencyGrant Number
NSFEAR-0606903
Gordon and Betty Moore FoundationUNSPECIFIED
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Caltech Tectonics Observatory208
Issue or Number:1
Record Number:CaltechAUTHORS:20140805-103825342
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140805-103825342
Official Citation:Robinson Cecil, Z. Saleeby, J. Saleeby, and K.A. Farley Pliocene–Quaternary subsidence and exhumation of the southeastern San Joaquin Basin, California, in response to mantle lithosphere removal Geosphere, February 2014, v. 10, p. 129-147, First published on January 14, 2014, doi:10.1130/GES00882.1
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:47967
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:05 Aug 2014 18:26
Last Modified:03 Oct 2019 06:58

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