Theirman Tin Mine, Blaxland Co., New South Wales, Australia
Latitude & Longitude (WGS84): | 32° 33' 55'' South , 146° 29' 2'' East |
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Latitude & Longitude (decimal): | -32.56530,146.48401 |
Age: | 485.4 ± 1.9 to 443.8 ± 1.5 Ma |
Geologic Time: | Ordovician |
Reference for age: | Gilligan, L.B., Suppel, D.W. (1993) Metallogenic Study and Mineral Deposit Data Sheets: Nymagee 1:250 000 Metallogenic Map (SI/55-2). Geological Survey of New South Wales, Sydney, 171 pages. |
Köppen climate type: | BSk : Cold semi-arid (steppe) climate |
A former small deposit.
Mineral List
2 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramRegional Geology
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
Late Ordovician - Early Ordovician 443.8 - 485.4 Ma ID: 925767 | Eulendool Formation Age: Ordovician (443.8 - 485.4 Ma) Stratigraphic Name: Eulendool Formation Description: Thick-bedded graded, parallel-laminated and ripple cross laminated, poorly sorted fine to coarse-grained, quartz sandstone and quartzite, interbedded with thinly bedded to massive mudstone and siltstone, minor massive to graded conglomerate Comments: sedimentary siliciclastic; synthesis of multiple published descriptions Lithology: Sedimentary siliciclastic Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia). [5] |
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