Curnamona Province - 3D Sedimentary Basins Model
Downloads
Name | Description | Download | Select |
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MESAJ058016-024.pdf | |||
GDP00033_PDF.zip | |||
GDP00033.zip | |||
Curnamona Province - 3D Sedimentary Basins Model |
About this record
Record No | mesac867 |
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Topic | Geoscientific Information |
Type of Resource | Model |
Category Type | |
Document Type | |
Contributor | Geological Survey of South Australia |
Sponsor | |
Geological Province | |
Mine Name | |
Stratigraphy | |
Commodity | |
Notes | |
Language | English |
Metadata Standard | ISO 19115-3 |
Use constraints | License |
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License | Creative Commons Attribution 4.0 |
Persistent identifier | https://pid.sarig.sa.gov.au/model/mesac867 |
Citation | Gouthas, G. Curnamona Province - 3D Sedimentary Basins Model https://pid.sarig.sa.gov.au/model/mesac867 |
Status | Completed |
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Maintenance and Update Frequency | |
Geographic Reference | GDA2020 (EPSG:7844) |
Geo bounding box | {"type":"Polygon","coordinates":[[[131.25915527,-31.71885399],[134.59899902,-31.71885399],[134.59899902,-29.43369774],[131.25915527,-29.43369774],[131.25915527,-31.71885399]]]} |
Purpose |
To aid in geological exploration. To aid in geological exploration. |
Lineage |
This model is presented as a 'proof of concept' only for the GOCAD software which the Geological Survey has recently begun to use, and its accuracy (spatial or otherwise) should not be relied upon for guiding exploration or other decision-making... This model is presented as a 'proof of concept' only for the GOCAD software which the Geological Survey has recently begun to use, and its accuracy (spatial or otherwise) should not be relied upon for guiding exploration or other decision-making processes. The horizontal accuracy of the geographic locations of drillholes is variable due to the method of spatial data capture (map, hand-held GPS, differential GPS, etc); likewise, the horizontal accuracy of the sedimentary basin boundaries is variable (due to the ways they were interpreted); and the vertical accuracy of the modelled formation surfaces, topographic and basement surfaces is variable due to resampling (topographic surface), interpretation (formation boundaries), and necessary gridding interpolation. |