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.
History
Year
1973
Thesis type
Doctoral thesis
Faculty/School
Wollongong University College
Language
English
Disclaimer
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.