Abstract
Bedding characteristics of the fluvial Hawkesbury Sandstone (Triassic) of the Sydney Basin are most readily explained in terms of a model of flood- and falling-stage vertical accretion derived from Coleman’s study of the Brahmaputra. This model suggests inadequacies in present concepts of 'braided stream' deposits based on observations made at low stage. A Brahmaputra model may be widely applicable to continental sheet sandstones. Copyright.
| Original language | English |
|---|---|
| Pages (from-to) | 275-283 |
| Number of pages | 9 |
| Journal | Journal of the Geological Society of Australia |
| Volume | 22 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 1 Jan 1975 |