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Production and loss of high-density batholithic root, southern Sierra Nevada, California

Saleeby, Jason and Ducea, Mihai and Clemens-Knott, Diane (2003) Production and loss of high-density batholithic root, southern Sierra Nevada, California. Tectonics, 22 (6). Art. No. 1064. ISSN 0278-7407. doi:10.1029/2002TC001374.

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Eclogites are commonly believed to be highly susceptible to delamination and sinking into the mantle from lower crustal metamorphic environments. We discuss the production of a specific class of eclogitic rocks that formed in conjunction with the production of the Sierra Nevada batholith. These high-density eclogitic rocks, however, formed by crystal-liquid equilibria and thus contrast sharply in their petrogenesis and environment of formation from eclogite facies metamorphic rocks. Experimental studies show that when hydrous mafic to intermediate composition assemblages are melted in excess of 1 GPa, the derivative liquids are typical of Cordilleran-type batholith granitoids, and garnet + clinopyroxene, which is an eclogitic mineralogy, dominate the residue assemblage. Upper mantle-lower crustal xenolith suites that were entrained in mid-Miocene volcanic centers erupted through the central Sierra Nevada batholith are dominated by such garnet clinopyroxenites, which are shown further by geochemical data to be petrogenetically related to the overlying batholith as its residue assemblage. Petrogenetic data on garnet pyroxenite and associated peridotite and granulite xenoliths, in conjunction with a southward deepening oblique crustal section and seismic data, form the basis for the synthesis of a primary lithospheric column for the Sierra Nevada batholith. Critical aspects of this column are the dominance of felsic batholithic rocks to between 35 and 40 km depths, a thick (∼35 km) underlying garnet clinopyroxenite residue sequence, and interlayered spinel and underlying garnet peridotite extending to ∼125 km depths. The peridotites appear to be the remnants of the mantle wedge from beneath the Sierran arc. The principal source for the batholith was a polygenetic hydrous mafic to intermediate composition lower crust dominated by mantle wedge-derived mafic intrusions. Genesis of the composite batholith over an ∼50 m.y. time interval entailed the complete reconstitution of the Sierran lithosphere. Sierra Nevada batholith magmatism ended by ∼80 Ma in conjunction with the onset of the Laramide orogeny, and subsequently, its underlying mantle lithosphere cooled conductively. In the southernmost Sierra-northern Mojave Desert region the subbatholith mantle lithosphere was mechanically delaminated by a shallow segment of the Laramide slab and was replaced by underthrust subduction accretion assemblages. Despite these Laramide events, the mantle lithosphere of the greater Sierra Nevada for the most part remained intact throughout much of Cenozoic time. A pronounced change in xenolith suites sampled by Pliocene-Quaternary lavas to garnet absent, spinel and plagioclase peridotites, whose thermobarometry define an asthenosphere adiabat, as well as seismic data, indicate that much of the remaining sub-Sierran lithosphere was removed in Late Miocene to Pliocene time. Such removal is suggested to have arisen from a convective instability related to high-magnitude extension in the adjacent Basin and Range province and to have worked in conjunction with the recent phase of Sierran uplift and a change in regional volcanism to more primitive compositions. In both the Mio-Pliocene and Late Cretaceous lithosphere removal events the base of the felsic batholith was the preferred locus of separation.

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Ducea, Mihai0000-0002-5322-0782
Additional Information:© 2003 by the American Geophysical Union. Received 20 February 2002; revised 21 March 2003; accepted 1 July 2003; published 18 November 2003. Support for this work was provided by NSF grants EAR-9526859, EAR-9815024, and EAR-0087347 (Saleeby) and EAR-0087125 (Ducea). Discussions and field excursions with L. T. Silver, R. W. Kistler, D. L. Anderson, P. D. Asimow, M. Gurnis, D. Helmberger, C. T. Lee, M. B. Wolf, P. J. Wyllie, G. Zandt, L. Zeng, and the entire Southern Sierra Continental Dynamics Project working group helped stimulate this work. Critical reviews from Peter Molnar and an unidentified reviewer are gratefully acknowledged. Drafting and technical assistance from Zorka Foster is gratefully acknowledged. Assistance in manuscript preparation by Kim Klotz is kindly acknowledged.
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Subject Keywords:Sierra Nevada, batholith petrogenesis, delamination, eclogites
Issue or Number:6
Record Number:CaltechAUTHORS:20130506-135423060
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Official Citation:Saleeby, J., M. Ducea, and D. Clemens-Knott (2003), Production and loss of high-density batholithic root, southern Sierra Nevada, California, Tectonics, 22, 1064, doi:10.1029/2002TC001374, 6
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:38298
Deposited By: Tony Diaz
Deposited On:16 May 2013 19:45
Last Modified:09 Nov 2021 23:36

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