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| Yass Sub-basin | |
|---|---|
| Name | Yass Sub-basin |
| Type | Sedimentary sub-basin |
| Location | Southern New South Wales, Australia |
| Coordinates | 35°N 149°E |
| Namedfor | Yass |
| Partof | Lachlan Fold Belt |
| Area | ~? km2 |
Yass Sub-basin is a sedimentary sub-basin in southern New South Wales, Australia, located within the broader Lachlan Fold Belt region near Yass, New South Wales. The sub-basin preserves a record of Palaeozoic marine and terrestrial deposition and later deformation tied to major orogenic and basin-forming events such as the Tabberabberan Orogeny and the Benambran Orogeny. It has attracted attention from Geological Survey of New South Wales researchers, industry geoscientists from Oil Search and Woodside Petroleum, and academic groups at the University of Sydney and the Australian National University.
The geology of the Yass Sub-basin is dominated by Palaeozoic stratigraphy that records interactions between the Murrumbidgee River drainage corridor, contemporaneous sediment sources in the Great Dividing Range, and marine incursions from basins comparable to the Sydney Basin and the Gunnedah Basin. Regional mapping by the Bureau of Mineral Resources and the Geological Society of Australia places the sub-basin within frameworks developed alongside studies of the Lachlan Orogen and the Tasman Orogeny. Metamorphic and plutonic associations correlate with granitic bodies similar to those studied in the Hill End Trough and around the Bathurst Region.
The Yass Sub-basin lies northwest of Canberra and southeast of Cowra, extending across parts of the Southern Tablelands and abutting the Sydney Basin margin. Its surface expression influences landforms from the Cotter River catchment to the river terraces of the Murrumbidgee River. Administrative overlays include the Yass Valley Council and nearby localities such as Gundaroo and Murrumbateman, while transport corridors like the Hume Highway and rail links facilitate access for fieldwork.
Stratigraphic columns from the sub-basin record sequences of siliciclastic and carbonate successions analogous to units described in the Molong Volcanic Belt and coal-bearing intervals compared with the Gunnedah Basin coal measures. Sedimentological interpretations reference turbidites, deltaic facies, and shallow marine shelves documented in studies by the Australian Journal of Earth Sciences and field campaigns led by the CSIRO. Fossil occurrences tied to Ordovician and Silurian assemblages have been correlated with biostratigraphic zones recognized in the Burrinjuck Dam area and by paleontologists associated with the Australian Museum.
The tectonic evolution of the Yass Sub-basin reflects convergence and accretion processes that built the Lachlan Fold Belt and were influenced by the regional plate interactions that include the remnants of the Paleo-Pacific Plate and motions preserved adjacent to the Lord Howe Rise. Structural studies highlight folding, thrusting, and strike-slip faulting comparable to structures mapped in the Canberra Region and the Cowra Structural Zone, with major faults traced by geophysical surveys conducted by the Geoscience Australia agency. Metamorphic grade variations and syn-tectonic intrusions relate to events documented in the Devonian and Carboniferous records.
Assessments of resource potential consider analogues from the Permian Basin-type coal and gas systems and petroleum systems examined in the Sydney Basin and Gunnedah Basin. Exploration efforts by companies such as Santos and joint ventures with the Australian Petroleum Production & Exploration Association have evaluated source rock maturity, reservoir quality, and trap integrity using seismic reflection data, borehole logs, and geochemical analyses similar to studies commissioned by the National Offshore Petroleum Safety and Environmental Management Authority. Mineral prospects include metal-bearing veins associated with granitic intrusions comparable to the Cadia-Ridgeway and Peak Hill districts.
Land use across the Yass Sub-basin involves mixed agriculture, viticulture near Hilltops, New South Wales-style districts, and conservation reserves managed in part by the NSW National Parks and Wildlife Service. Water resource management links to the Murrumbidgee Irrigation Area and environmental flow studies coordinated with the Murray–Darling Basin Authority. Biodiversity inventories conducted by teams from the Australian National Botanic Gardens and local councils note habitats for native species whose conservation status is considered under instruments like the Environment Protection and Biodiversity Conservation Act 1999.
Historical exploration began with reconnaissance mapping by the Bureau of Mineral Resources in the mid-20th century and progressed through targeted seismic campaigns and drilling programs supported by the Department of Primary Industries, New South Wales and academic collaborations involving the University of New England and the University of Wollongong. Key publications in journals such as the Australian Journal of Earth Sciences and conference proceedings of the Geological Society of Australia document stratigraphic revisions, geochronology, and tectonic syntheses. Ongoing research integrates data from the Australian Earthquake Monitoring Network and modern remote sensing by the Commonwealth Scientific and Industrial Research Organisation.
Category:Geology of New South Wales