Crustal structure of the northwestern Basin and Range Province and its transition to unextended volcanic plateaus-Reference-Cited by-同舟云学术

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Crustal structure of the northwestern Basin and Range Province and its transition to unextended volcanic plateaus

Published:2007-02 Issue:2 Volume:8 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Lerch D. W.,Klemperer S. L.¹,Glen J. M. G.²,Ponce D. A.²,Miller E. L.³,Colgan J. P.²

Affiliation:

1. Department of Geophysics; Stanford University; Mitchell Building 353,; Stanford; California; 94305; USA

2. U.S. Geological Survey; MS 989, 345 Middlefield Road,; Menlo Park; California; 94025; USA

3. Department of Geological and Environmental Sciences; Stanford University; Building 320,; Stanford; California; 94305; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference85 articles.

1. Overview of the COCORP 40°N transect, western United States: The fabric of an orogenic belt;Allmendinger;Geol. Soc. Am. Bull.,1987

2. Transition from slab to slabless: Results from the 1993 Mendocino Triple Junction seismic experiment;Beaudoin;Geology,1996

3. Limited extension during peak Tertiary volcanism, Great Basin of Nevada and Utah;Best;J. Geophys. Res.,1991

4. Cascades and Intermountain West, Mem. N. M. Bur. Mines Miner. Resour.;Best,1989

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