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Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California

Saleeby, Jason and Saleeby, Zorka (2019) Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California. Geosphere, 15 (4). pp. 1164-1205. ISSN 1553-040X. doi:10.1130/GES02052.1. https://resolver.caltech.edu/CaltechAUTHORS:20190621-153801690

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Abstract

This paper presents a new synthesis for the late Cenozoic tectonic, paleogeographic, and geomorphologic evolution of the southern Sierra Nevada and adjacent eastern San Joaquin Basin. The southern Sierra Nevada and San Joaquin Basin contrast sharply, with the former constituting high-relief basement exposures and the latter constituting a Neogene marine basin with superposed low-relief uplifts actively forming along its margins. Nevertheless, we show that Neogene basinal conditions extended continuously eastward across much of the southern Sierra Nevada, and that during late Neogene–Quaternary time, the intra-Sierran basinal deposits were uplifted and fluvially reworked into the San Joaquin Basin. Early Neogene normal-sense growth faulting was widespread and instrumental in forming sediment accommodation spaces across the entire basinal system. Upon erosion of the intra-Sierran basinal deposits, structural relief that formed on the basement surface by the growth faults emerged as topographic relief. Such “weathered out” fossil fault scarps control much of the modern southern Sierra landscape. This Neogene high-angle fault system followed major Late Cretaceous basement structures that penetrated the crust and that formed in conjunction with partial loss of the region’s underlying mantle lithosphere. This left the region highly prone to surface faulting, volcanism, and surface uplift and/or subsidence transients during subsequent tectonic regimes. The effects of the early Neogene passage of the Mendocino Triple Junction were amplified as a result of the disrupted state of the region’s basement. This entailed widespread high-angle normal faulting, convecting mantle-sourced volcanism, and epeirogenic transients that were instrumental in sediment dispersal, deposition, and reworking patterns. Subsequent phases of epeirogenic deformation forced additional sediment reworking episodes across the southern Sierra Nevada–eastern San Joaquin Basin region during the late Miocene break-off and west tilt of the Sierra Nevada microplate and the Pliocene–Quaternary loss of the region’s residual mantle lithosphere that was left intact from the Late Cretaceous tectonic regime. These late Cenozoic events have left the high local-relief southern Sierra basement denuded of its Neogene basinal cover and emergent immediately adjacent to the eastern San Joaquin Basin and its eastern marginal uplift zone.


Item Type:Article
Related URLs:
URLURL TypeDescription
https://doi.org/10.1130/GES02052.1DOIArticle
Additional Information:© 2019 The Authors. This paper is published under the terms of the CC-BY-NC license. We gratefully acknowledge support from the Gordon and Betty Moore Foundation and the Division of Geological and Planetary Sciences, California Institute of Technology. We acknowledge helpful discussions, sharing of resources, and field excursions with Timothy Elam, Jan Gillespie, A.F. Glazner, S.A. Graham, W.D. Kleck, Larry Knauer, J.S. Lewis, S.A. Reid, F.J. Sousa, and J.R. Unruh. Analyses performed in the isotope geochemistry laboratories of K.A. Farley (California Institute of Technology), G.E. Gehrels and Mihai Ducea (University of Arizona, Tucson), and M. Cosca (U.S. Geological Survey, Denver, Colorado) were of critical importance for this study. We also acknowledge the California Division of Oil and Gas online oil well file database and the California State University, Bakersfield oil well core repository. Co-author J.S. acknowledges J.C. Crowell’s influence on pursuing in detail basement-cover strata relationships in working out the Cenozoic tectonics of the southern California region.
Funders:
Funding AgencyGrant Number
Gordon and Betty Moore FoundationUNSPECIFIED
Caltech Division of Geological and Planetary SciencesUNSPECIFIED
Issue or Number:4
DOI:10.1130/GES02052.1
Record Number:CaltechAUTHORS:20190621-153801690
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20190621-153801690
Official Citation:Jason Saleeby, Zorka Saleeby; Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California. Geosphere ; 15 (4): 1164–1205. doi: https://doi.org/10.1130/GES02052.1
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:96641
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:22 Jun 2019 12:37
Last Modified:16 Nov 2021 17:22

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