Caliche pseudo- anticlines in the Fitzroy Basin, Western Australia

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ID: 297991
1961
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Abstract
The caliche pseudoanticlines form a series of low ridges developed in competent limestone beds. Arching of the beds is considered to have been associated with caliche formation. Sustained high temperatures probably are an important factor in the buckling process. Recognition of the structures is significant not only for geomorphic investigations but also for stratigraphic mapping.
Reference Key
openalex_W2331841192 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. N. Jennings, M. M. Sweeting
Journal american journal of science
Year 1961
DOI
10.2475/ajs.259.8.635
URL
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