| Deposit ID | 10023302 |
|---|---|
| MRDS ID | I000145 |
| Record type | Site |
| Current site name | Limestone Creek |
| Geographic coordinates: | 145.7818, -41.26278 (WGS84) |
|---|---|
| Location accuracy | 10000(meters) |
| Relative position | 1.5 MILES EAST OF HAMPSHIRE, 27 KM SOUTHWEST OF BURNIE. |
Political divisions (FIPS codes)
Tasmania(province)
Australia(country)
Australia(continent)
Land(continent)
| Country | State |
|---|---|
| Australia | Tasmania |
| Commodity | Importance |
|---|---|
| Wollastonite | Primary |
| Materials | Type of material |
|---|---|
| Wollastonite | Ore |
| Calcite | Gangue |
| Diopside | Gangue |
| Plagioclase | Gangue |
| Pyrrhotite | Gangue |
| Quartz | Gangue |
| Result | WOLLASTONITE GRAIN SIZE AVERAGES 0.02 INCH, BUT UP TO 0.5 INCH IN SIZE. |
|---|
| Model code | 65 |
|---|---|
| USGS model code | 18g |
| Deposit model name | Skarn wollastonite |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Chemical Sediment > Chert |
| (1) | 145.7818, -41.26278 |
|---|
| Strike | SOUTH |
|---|---|
| Dip | 12W |
| Thickness | 0.91M |
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000145 |
ANDREWS, R.W., 1970, WOLLASTONITE: LONDON, INSTITUTE OF GEOLOGICAL SCIENCES, P. 51-52.
JOHNS, R.K., 1986, LETTER TO THE EDITOR: INDUSTRIAL MINERALS, NO. 225, P. 19.
ANDREWS, 1970.
| Subject category | Comment text |
|---|---|
| Deposit | BANDS OF WOLLASTONITE ROCK OCCUR INTERBEDDED WITH LIMESTONE AND CHERT. THE BANDS OF WOLLASTONITE RANGE FROM 2 INCHES TO 3 FT THICK, STRIKE 165-195 DEGREES, AND DIP WEST AT 10-15 DEGREES. UP TO 6 FT OF OVERBURDEN IS PRESENT. AVERAGE GRADE IS 30%, BUT COULD BE INCREASED TO 37% BY REJECTING THE CHERT BANDS. 80% OF THE ROCK IS WOLLASTONITE PLUS QUARTZ. PYRRHOTITE FORMS 5-10% OF THE ORE. DEPOSIT IS A ROOF PENDENT IN DEVONIAN GRANITE, PARTLY OVERLAIN BY TERTIARY BASALT. THE WOLLASTONITE-QUARTZ ROCK CONTAINS 5-10% PYRRHOTITE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-89 | Orris, Greta J. | U.S. Geological Survey | |
| Updater | 01-NOV-92 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.