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Epeirogenic transients related to mantle lithosphere removal in the southern Sierra Nevada region, California: Part II. Implications of rock uplift and basin subsidence relations

Saleeby, J. and Saleeby, Z. and Le Pourhiet, L. (2013) Epeirogenic transients related to mantle lithosphere removal in the southern Sierra Nevada region, California: Part II. Implications of rock uplift and basin subsidence relations. Geosphere, 9 (3). pp. 394-425. ISSN 1553-040X. http://resolver.caltech.edu/CaltechAUTHORS:20130725-084053637

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Abstract

We investigate the putative Pliocene–Quaternary removal of mantle lithosphere from beneath the southern Sierra Nevada region using a synthesis of subsidence data from the Great Valley, and geomorphic relations across the Sierra Nevada. These findings are used to test the results and predictions of thermomechanical modeling of the lithosphere removal process that is specific to the Sierra Nevada, as presented in an accompanying paper referenced here as Part I. Our most successful thermomechanical model and the observational data that it explains are further bundled into an integrated physiographic evolution–geodynamic model for the three-dimensional epeirogenic deformation field that has affected mainly the southern Sierra Nevada–San Joaquin Basin region as a result of underlying mantle lithosphere removal. The coupled Sierra Nevada mountain range and Great Valley basin are recognized as a relatively rigid block (Sierra Nevada microplate) moving within the San Andreas–Walker Lane dextral plate juncture system. Our analysis recognizes that the Sierra Nevada possessed kilometer-scale local and regional paleotopographic relief, and that the Great Valley forearc basin possessed comparable structural relief on its principal stratigraphic horizons, both dating back to the end of Cretaceous time. Such ancient paleorelief must be accounted for in considering late Cenozoic components of uplift and subsidence across the microplate. We further recognize that Cenozoic rock and surface uplift must be considered from the perspectives of both local epeirogeny driven by mantle lithosphere removal, and regional far-field–forced epeirogeny driven by plate tectonics and regional upper-mantle buoyancy structure. Stratigraphic relations of Upper Cretaceous and lower Cenozoic marine strata lying on northern and southern Sierra Nevada basement provide evidence for near kilometer-scale rock uplift in the Cenozoic. Such uplift is likely to have possessed positive, and then superposed negative (subsidence) stages of relief generation, rendering net regional rock and surface uplift. Accounting for ancient paleorelief and far-field–driven regional uplift leaves a residual pattern whereby ∼1200 m of southeastern Sierra crest rock and similar surface uplift, and ∼700 m of spatially and temporally linked tectonic subsidence in the southern Great Valley were required in the late Cenozoic by mantle lithosphere removal. These values are close to the predictions of our modeling, but application of the model results to the observed geology is complicated by spatial and temporal variations in the regional tectonics that probably instigated mantle lithosphere removal, as well as spatial and temporal variations in the observed uplift and subsidence patterns. Considerable focus is given to these spatial-temporal variation patterns, which are interpreted to reflect a complex three-dimensional pattern resulting from the progressive removal of mantle lithosphere from beneath the region, as well as its epeirogenic expressions. The most significant factor is strong evidence that mantle lithosphere removal was first driven by an east-to-west pattern of delamination in late Miocene–Pliocene time, and then rapidly transitioned to a south-to-north pattern of delamination in the Quaternary.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1130/GES00816.1DOIArticle
http://geosphere.gsapubs.org/content/9/3/394.abstractPublisherArticle
http://geosphere.geoscienceworld.org/content/9/3/394PublisherArticle
Additional Information:© 2013 Geological Society of America. Received 2 May 2012; Revision received 23 January 2013; Accepted 19 February 2013; Published online 17 April 2013. This research was supported by National Science Foundation grants EAR-0230383 and EAR-0606903, a grant from the George and Betty Moore Foundation, and Faculty Research Funds from the Université Pierre et Marie Curie, France. This is Caltech Tectonics Observatory Contribution 142. Conversations and field excursions with C.J. Busby, J. Gillespe, S.A. Graham, J.S. Lewis, D.D. Miller, K. Putirka, A.G. Sylvester, and J. Wakabayashi helped enrich this work. We also acknowledge the editorial efforts of J.R. Unruh, C.H. Jones, and D.L. Harry in greatly improving the clarity of this publication.
Group:Caltech Tectonics Observatory
Funders:
Funding AgencyGrant Number
NSFEAR-0230383
NSFEAR-0606903
Gordon and Betty Moore FoundationUNSPECIFIED
Université Pierre et Marie Curie Faculty Research FundsUNSPECIFIED
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Other Numbering System NameOther Numbering System ID
Caltech Tectonics Observatory142
Record Number:CaltechAUTHORS:20130725-084053637
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20130725-084053637
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:39575
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:12 Aug 2013 21:40
Last Modified:12 Aug 2013 21:40

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