Year

1973

Degree Name

Doctor of Philosophy

Department

Wollongong University College

Abstract

In the Macquarie Syncline and a number of other areas of the Sydney Basin there is an apparent relationship between the thickness of some formations and the present-day structure of the Basin. Trend-surface analysis of borehole information has been used to quantitatively analyse both the structure and thickness data of the Moon Island Beach Sub-group into regional and local components. The vertical variation of the Sub-group has been analysed using Markov Chain analysis.

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Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong.