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Janet L Slate

Biographic Data

ID6417370
NAMEJanet L Slate
GIVEN NAMESJanet L
FAMILY NAMESlate
SIGNATURESLATE J L
AFFILIATIONSUniversity of Arizona
ORCID0000-0002-2870-9068
VERIFIEDYes
TOTAL WORKS7
TOTAL CITATIONS0
WORKS AS AUTHOR7
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1985
LATEST PUBLICATION YEAR2008
H-INDEX0
  • Global tephra studies

    Open Access•Duane G Froese, David J Lowe et al.•ARTICLE•Quaternary International•2008

  • Tephrochronology

    Open Access•Janet L Slate•ARTICLE•Quaternary International•2008

  • Hydromorphic-soil origin of carbonate glaebules in pliocene paleosols of southeastern Arizona

    Open Access•Janet L Slate•ARTICLE•Quaternary International•1998

  • Buried carbonate paleosols developed in Pliocene-Pleistocene deposits of the Pasco Basin, south-central Washington, U.S.A

    Open Access•Janet L Slate•ARTICLE•Quaternary International•1996

  • Fission-Track Age (400,000 yr) of the Rockland Tephra, Based on Inclusion of Zirco Grains Lacking Fossil Fission Tracks

    Open Access•C Meyer, C E Meyer et al.•ARTICLE•Quaternary Research•1991

    A zircon fission-track age of about 400,000 yr B.P. has been determined for the Rockland tephra, a widespread pyroclastic layer in northern California and western Nevada. New ages of zircon separates from both proximal and distal exposures of this layer range from 370,000 to 460,000 yr; ages of the best material provide a narrower range, from 370,000 yr for unwelded ash-flow tuff to 420,000 yr for distal air-fall ash that appears to be uncontamin…

  • Soil-Carbonate Genesis in the Pinacate Volcanic Field, Northwestern Sonora, Mexico

    Open Access•Janet L Slate, William B Bull et al.•ARTICLE•Quaternary Research•1991

    Uranium-series methods were used to date and evaluate pedogenic CaCO 3 genesis in the Pinacate volcanic field, northwestern Sonora, Mexico. Soils are developed in eolian deposits on lava flows. 230 Th/ 234 U dates of pedogenic carbonate are mininum soil ages because of (1) the time needed to yield clasts from flows and to accrete enough carbonate to sample, (2) subsequent additions of uranium, and (3) continued solution and reprecipitation of car…

  • Correlation of the Rockland Ash Bed, a 400,000-Year-Old Stratigraphic Marker in Northern California and Western Nevada, and Implications for Middle Pleistocene Paleogeography of Central California

    Open Access•Andrei M Sarna-Wojcicki, Andrei M Sarna‐Wojcicki et al.•ARTICLE•Quaternary Research•1985

    Outcrops of an ash bed at several localities in northern California and western Nevada belong to a single air-fall ash layer, the informally named Rockland ash bed, dated at about 400,000 yr B.P. The informal Rockland pumice tuff breccia, a thick, coarse, compound tephra deposit southwest of Lassen Peak in northeastern California, is the near-source equivalent of the Rockland ash bed. Relations between initial thickness of the Rockland ash bed an…

No prominent works on this page.

  • Correlation of the Rockland Ash Bed, a 400,000-Year-Old Stratigraphic Marker in Northern California and Western Nevada, and Implications for Middle Pleistocene Paleogeography of Central California

    Open Access•Andrei M Sarna-Wojcicki, Andrei M Sarna‐Wojcicki et al.•ARTICLE•Quaternary Research•1985

    Outcrops of an ash bed at several localities in northern California and western Nevada belong to a single air-fall ash layer, the informally named Rockland ash bed, dated at about 400,000 yr B.P. The informal Rockland pumice tuff breccia, a thick, coarse, compound tephra deposit southwest of Lassen Peak in northeastern California, is the near-source equivalent of the Rockland ash bed. Relations between initial thickness of the Rockland ash bed an…

  • Fission-Track Age (400,000 yr) of the Rockland Tephra, Based on Inclusion of Zirco Grains Lacking Fossil Fission Tracks

    Open Access•C Meyer, C E Meyer et al.•ARTICLE•Quaternary Research•1991

    A zircon fission-track age of about 400,000 yr B.P. has been determined for the Rockland tephra, a widespread pyroclastic layer in northern California and western Nevada. New ages of zircon separates from both proximal and distal exposures of this layer range from 370,000 to 460,000 yr; ages of the best material provide a narrower range, from 370,000 yr for unwelded ash-flow tuff to 420,000 yr for distal air-fall ash that appears to be uncontamin…

  • Soil-Carbonate Genesis in the Pinacate Volcanic Field, Northwestern Sonora, Mexico

    Open Access•Janet L Slate, William B Bull et al.•ARTICLE•Quaternary Research•1991

    Uranium-series methods were used to date and evaluate pedogenic CaCO 3 genesis in the Pinacate volcanic field, northwestern Sonora, Mexico. Soils are developed in eolian deposits on lava flows. 230 Th/ 234 U dates of pedogenic carbonate are mininum soil ages because of (1) the time needed to yield clasts from flows and to accrete enough carbonate to sample, (2) subsequent additions of uranium, and (3) continued solution and reprecipitation of car…

  • Buried carbonate paleosols developed in Pliocene-Pleistocene deposits of the Pasco Basin, south-central Washington, U.S.A

    Open Access•Janet L Slate•ARTICLE•Quaternary International•1996

  • Hydromorphic-soil origin of carbonate glaebules in pliocene paleosols of southeastern Arizona

    Open Access•Janet L Slate•ARTICLE•Quaternary International•1998

  • Global tephra studies

    Open Access•Duane G Froese, David J Lowe et al.•ARTICLE•Quaternary International•2008

  • Tephrochronology

    Open Access•Janet L Slate•ARTICLE•Quaternary International•2008

Geology and Paleoclimatology Research (7 works) · Geochemistry (4 works) · Geology (4 works) · Paleontology (4 works) · Volcano (4 works) · Carbonate (3 works) · Fluvial (3 works) · Geological and Geochemical Analysis (3 works) · Geology (3 works) · Geomorphology (3 works)

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