COMPUTER ANALYSIS OF ORIENTATION DATA IN STRUCTURAL GEOLOGY.

Abstract

Three-dimensional orientation data can be simplified by transforming them to refer to axes related to the symmetry of the distribution. Three uncorrelated scalar variates are generated by the transformation. Each of the scalar variates generally has direct geological significance. Each variate can be described individually by the usual statistical parameters. Thus, the orientation, tightness, asymmetry, shape and size of folds can be measured statistically; first, in the direction of greatest buckling; second, parallel to the fold axis. The degree to which a fold is cylindrical or conical in form can be estimated by a least-squares method. A Fortran IV program has been written to perform the computations. A consideration of the spatial variation of the parameters allows various types of folding to be discriminated quantitatively, and permits the testing of hypotheses of the origin of folding. (Author)

Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1964
Accession Number
AD0608892

Entities

People

  • T. Victor Loudon

Organizations

  • Northwestern University

Tags

DTIC Thesaurus Topics

  • Asymmetry
  • Attitude (Inclination)
  • Buckling
  • Computations
  • Computers
  • Geology
  • Hypotheses
  • Least Squares Method
  • Mathematics
  • Orientation (Direction)
  • Structural Geology
  • Symmetry
  • Three Dimensional
  • Tightness

Fields of Study

  • Geology

Readers

  • Approximation Theory.
  • Regression Analysis.
  • Structural Dynamics.