AusGeol.orgConran4
Site:
Conran4
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Map
3D Model:
Description:
Disrupted isoclinal fold hinge in turbiditic metasediments of the Ordovician Pinnak Sandstone. Axial planar cleavage is well developed in the hinge of the fold. Cape Conran, Vic.
| Capture Date: | July 18, 2015, 3:10 p.m. |
| Latitude: | -37.80046000000 degrees |
| Longitude: | 148.74255000000 degrees |
| Elevation: | NA |
| Visualisation Type: | 3D |
| Location Accuracy: | 5 metres |
Keywords:
- turbidite
- isoclinal fold
- cleavage
- structure
| turbidite | |
|---|---|
| Form Type: | bedded |
| Description: | thinly bedded turbidite units consisting of fine sandstone and siltstone. Intensely deformed |
| Min Geological Age: | Ordovician |
| Max Geological Age: | Ordovician |
| Min Numerical Age: | 458.000 |
| Max Numerical Age: | 467.000 |
| Strat No: | 23907 |
| Supergroup: | |
| Group: | Adaminaby Group |
| Subgroup: | |
| Formation: | Pinnak Sandstone |
| Member: | |
| Province: | Lachlan Orogen |