Movement and diffusion of pore fluids in Owens Lake sediments from core OL-92 as shown by salinity and deuterium-hydrogen ratios

Irving I. Friedman; James L. Bischoff; Craig A. Johnson; Scott W. Tyler; Jeffrey P. Fitts

doi:10.1130/0-8137-2317-5.49

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Movement and diffusion of pore fluids in Owens Lake sediments from core OL-92 as shown by salinity and deuterium-hydrogen ratios

Author(s)

Irving I. Friedman

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;

James L. Bischoff

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;

Craig A. Johnson

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;

Scott W. Tyler

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;

Jeffrey P. Fitts

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Doi:

https://doi.org/10.1130/0-8137-2317-5.49

Published:

January 01, 1997

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GSA Special Papers

An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California

Author(s)

Geological Society of America

Volume

317

DOI:

https://doi.org/10.1130/SPE317

Geological Society of America

ISBN print:

9780813723174

Publication date:

January 01, 1997

Movement and diffusion of pore fluids in Owens Lake sediments from core OL-92 as shown by salinity and deuterium-hydrogen ratios

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Contents

An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California

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References

Related

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Movement and diffusion of pore fluids in Owens Lake sediments from core OL-92 as shown by salinity and deuterium-hydrogen ratios

Figures & Tables

Contents

An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California

GeoRef

References

Related

Citing Books via

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