Lower Eocene alluvial paleosols (Willwood Formation, Northwest Wyoming, U.S.A.) and their significance for paleoecology, paleoclimatology, and basin analysis-Reference-Cited by-同舟云学术

Lower Eocene alluvial paleosols (Willwood Formation, Northwest Wyoming, U.S.A.) and their significance for paleoecology, paleoclimatology, and basin analysis

Published:1981-01 Issue: Volume:34 Page:1-30
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Bown Thomas M.,Kraus Mary J.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference91 articles.

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2. Ferruginous concretions around root channels in clay and fine sand deposits;Alhonen;Bull. Geol. Soc. Finl.,1975

3. Cornstone;Allen;Geol. Mag.,1960

4. Studies in fluviatile sedimentation: implications of pedogenic carbonate units, lower Old Red Sandstone, Anglo-Welsh outcrop;Allen;Geol. J.,1974

5. Studies in fluviatile sedimentation: an exploratory quantitative model for the architecture of avulsion-controlled alluvial suites;Allen;Sediment. Geol.,1978

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