Geologists: And their contribution to Australia |
| |
| Authors: | F Canavan |
| |
| Institution: | Broken Hill Proprietary Co. Ltd , G.P.O. Box 86A, Melbourne, Vic., 3001 |
| |
| Abstract: | Abstract Eight sets of stratigraphic layers and igneous rocks are the basis for the recognition of eight tectonic periods, TP1‐TP8, in the history of the New England and Yarrol Orogens from the Devonian to the opening of the Tasman Sea in the Late Cretaceous. The opening of the Tasman Sea caused the removal of an eastern section of the New England Orogen to form parts of the Lord Howe Rise and Norfolk Ridge. The Gwydir‐Calliope and Kuttung volcanic arc systems of TP1 and TP2 in the Devonian and Carboniferous were possibly W‐facing, and probably formed far to the NE of their present positions relative to the Lachlan Orogen. They moved SW as they developed, and in the latest Carboniferous or earliest Permian were cut obliquely by the Mooki Fault on which there was a dextral strike‐slip of about 500 km before the Kuttung volcanic arc became extinct. In the Late Carboniferous a narrow region on the E side of the Peel Fault was elevated to form the Campbell High which was intruded by the Bundarra Plutonic Suite and has probably remained elevated since then. Plutons of similar ages were intruded into a high to the E of the Bowen Basin (and the northern part of the Mooki Fault). The two highs and the intrusives in them divided the Yarrol Belt of the Yarrol Orogen from the Tamworth Belt of the New England Orogen, and the two belts have developed in different ways since the Visean. In Latest Carboniferous to Early Permian there was a major tectonic change and the Gympie‐Brook Street volcanic arc developed. The New England Orogen was in a back arc setting and broke into a mosaic of microplates, the relative motions between them being accompanied by deposition of diamictites, by metamorphism, by folding on W to NW trending axes, and by the intrusion of the Hillgrove Plutonic Suite. Further W, sediments of the Sydney, Gunnedah and Bowen basins were deposited above the Mooki Fault System and above the two segments of the Kuttung arc system that had been displaced along the Mooki Fault System. |
| |
| Keywords: | New England Orogen tectonic model |
|
|
