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Science 15 September 2000: Vol. 289. no. 5486, pp. 1912 - 1916 DOI: 10.1126/science.289.5486.1912
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Reports
Osmium Isotopic Evidence for Mesozoic Removal of Lithospheric Mantle Beneath the Sierra Nevada, California
Cin-Ty Lee,1*
Qingzhu Yin,1
Roberta L. Rudnick,1
John T. Chesley,2
Stein B. Jacobsen1
Thermobarometric and Os isotopic data for peridotite
xenoliths from late Miocene and younger lavas in the Sierra Nevada
reveal that the lithospheric mantle is vertically stratified: the
shallowest portions (<45 to 60 kilometers) are cold (670° to
740°C) and show evidence for heating and yield Proterozoic Os model
ages, whereas the deeper portions (45 to 100 kilometers) yield
Phanerozoic Os model ages and show evidence for extensive cooling from
temperatures >1100°C to 750°C. Because a variety of isotopic
evidence suggests that the Sierran batholith formed on preexisting
Proterozoic lithosphere, most of the original lithospheric mantle
appears to have been removed before the late Miocene, leaving only a
sliver of ancient mantle beneath the crust.
1 Department of Earth and Planetary Sciences,
Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA.
2 Department of Geological Sciences, Gould-Simpson
Building, Building 77, University of Arizona, Tucson, AZ 85712, USA.
*
To whom correspondence should be addressed. E-mail:
ctlee{at}eps.harvard.edu
Present address: Department of Geology, University of
Maryland, College Park, MD 20742, USA.
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- G. L. Farmer, A. F. Glazner, and C. R. Manley (2002)
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