Abstract
The effect of mineral grain shape and specific gravity on trend-surface gradients of mineral concentrations was investigated. Trend surfaces were computed by least-square procedures, and the influence of different combinations of grain shape and specific gravity was checked using a set of linear hypotheses in the form of an analysis of variance.
Similar content being viewed by others
Reference
Wilks, S. S., 1962, Mathematical statistics (2nd ed.): John Wiley & Sons, New York, 284 p. (Russian transl. 1967).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Romanova, M.A. Checking linear hypothesis in factor evaluation by use of trend-surface gradients in the investigation of eolian deposits. Mathematical Geology 2, 231–240 (1970). https://doi.org/10.1007/BF02312472
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF02312472