Anisotropy of magnetic susceptibility as a tool for recognizing core deformation: reevaluation of the paleomagnetic record of Pleistocene sediments from drill hole OL-92, Owens Lake, California

Author:

Rosenbaum Joseph,Reynolds Richard,Smoot Joseph,Meyer Robert

Publisher

Elsevier BV

Reference19 articles.

1. Paleomagnetic excursions as magneto-stratigraphic horizons: A cautionary note;Verosub;Science,1975

2. Magnetic susceptibility anisotropy as an indicator of sedimentary fabric in the Gurnigel Flysch;Channell;Eclog. Geol. Helv.,1979

3. Anomalous magnetic fabric in sediments which record an apparent geomagnetic field excursion;Marino;Nature,1978

4. G.I. Smith, J.L. Bischoff, Core OL-92 from Owens Lake: Project rationale, geologic setting, drilling procedures, and summary, in: G.I. Smith, J.L. Bischoff (Eds.), An 800,000-year Geologic and Climatic Record from Owens Lake, California: Core OL-92, Geol. Soc. Am. Spec. Pap. 317, 1997, pp. 1–8.

5. J.P. Smoot, Sedimentary features in core OL-92, 0.9–82.5 m depth, Owens Lake, California, in: J.L. Bischoff (Ed.), The Last Interglaciation at Owens Lake, California, U.S. Geol. Surv. OFR 98-132, 1998, pp. 6–34.

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