Tertiary uplift of the Mt. Doonerak antiform, central Brooks Range, Alaska: Apatite fission-track evidence from the Trans-Alaska crustal ransect

Paul B. O'Sullivan; Thomas E. Moore; John M. Murphy

doi:10.1130/0-8137-2324-8.179

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Tertiary uplift of the Mt. Doonerak antiform, central Brooks Range, Alaska: Apatite fission-track evidence from the Trans-Alaska crustal ransect

Author(s)

Paul B. O'Sullivan

School of Earth Sciences, La Trobe University, Bundoora, Victoria 3083, Australia

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;

Thomas E. Moore

U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025

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;

John M. Murphy

Department of Geology/Geophysics, University of Wyoming, Laramie, Wyoming 82071

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Doi:

https://doi.org/10.1130/0-8137-2324-8.179

Published:

August 01, 1998

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GSA Special Papers

Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska

Author(s)

Geological Society of America

Volume

324

DOI:

https://doi.org/10.1130/SPE324

Geological Society of America

ISBN print:

9780813723242

Publication date:

August 01, 1998

Tertiary uplift of the Mt. Doonerak antiform, central Brooks Range, Alaska: Apatite fission-track evidence from the Trans-Alaska crustal ransect

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Contents

Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska

GeoRef

References

Related

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Tertiary uplift of the Mt. Doonerak antiform, central Brooks Range, Alaska: Apatite fission-track evidence from the Trans-Alaska crustal ransect

Figures & Tables

Contents

Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska

GeoRef

References

Related

Citing Books via

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