Abstract
Stretching of the continental crust in the Basin and Range, western USA1, has more than doubled the surface area of the central province2. But it is unknown whether stretching affects the entire column of lithosphere down to the convecting mantle, if deep extension occurs offset to the side, or if deeper layers are entirely decoupled from the upper crust3,4. The central Basin and Range province is unusual, compared with its northern and southern counterparts: extension began later1; volcanism was far less voluminous5; and the unique geochemistry of erupted basalts6,7,8,9,10,11 suggests a long-preserved mantle source. Here we use seismic data and isostatic calculations to map lithospheric thickness in the central Basin and Range. We identify an isolated root of ancient mantle lithosphere that is ∼125 km thick, providing geophysical confirmation of a strong, cold mantle previously inferred from geochemistry6,7,8. We suggest that the root caused the later onset of extension and prevented the eruption of voluminous volcanism at the surface. We infer that the root initially pulled away from the Colorado Plateau along with the crust, but then was left behind intact during extension across Death Valley to the Sierra Nevada. We conclude that the upper crust is now decoupled from and moving relative to the root.
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Acknowledgements
We thank P. Luffi for providing density, entropy, and thermobarometry calculations; B. Schmandt for providing a tomographic model; G. L. Farmer for discussions; B. Wernicke for comments; A. Dean, M. Pettit, J. Ball and C. Vockrodt for assistance with data processing and plots; and the US National Science Foundation for support. A. Dean and M. Pettit were funded in part by the Incorporated Research Institutions for Seismology’s summer internship program. Maps were produced with GMT.
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A.S. and G.B. initiated the seismic data exchange. G.B. contributed SGBDSN data and tomographic models. A.S. assisted with initial seismic data acquisition and analysis. C.J. pointed out the geographic correspondence between the isostatic results and basalt geochemistry and contributed the compilation of refraction experiment results. V.S-P. performed the seismic and isostatic analysis and wrote the paper. All authors discussed the results and commented on the paper.
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Schulte-Pelkum, V., Biasi, G., Sheehan, A. et al. Differential motion between upper crust and lithospheric mantle in the central Basin and Range. Nature Geosci 4, 619–623 (2011). https://doi.org/10.1038/ngeo1229
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DOI: https://doi.org/10.1038/ngeo1229
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