11088627
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU11088627
| Property | Value |
|---|---|
| id | 11088627 |
| igsn | 10.60494/dcrp-1m58 |
| sample_id | TH141 |
| eno | 1083074 |
| sampling_feature_name | TH141 |
| sampling_feature_type | field site |
| sample_type | unknown |
| sampling_method | unknown |
| material_class | rock |
| stratigraphic_unit | Tick Hill syn-D3 pegmatite |
| geological_province | None |
| sample_remark | felsic pegmatite vein in the north wall of the pit, where it transects the dominant composite S1-2 fabric in biotite-chlorite schist at a low angle across sharp intrusive boundaries. The pegmatite intruded along the main D3 shear zone that forms the host to mineralization, and is associated with an array of en echelon quartz veins consistent with a normal-sinistral sense of movement, i.e. the pegmatite will provide an age for D3 normal faulting. Sample TH141 is not foliated and largely consists of coarse-grained albite and K-feldspar with subordinate quartz and minor biotite. Much of the feldspar was strongly altered to albite, epidote, sericite and clay minerals while biotite was replaced by chlorite. |
| earth_materials | Y |
| structural_measurements | None |
| inorganic_geochemistry | None |
| organic_geochemistry | None |
| geochronology | None |
| isotope_groups | None |
| hydrochemistry | None |
| rock_properties | None |
| mineralogy | None |
| thin_sections | None |
| repository_samples | None |
| mineral_deposit_samples | Y |
| mineral_deposit_waste_samples | None |
| linked_files | None |
| other_geological_data | None |
| project_name | None |
| gda94_longitude | 139.9260336 |
| gda94_latitude | -21.6456144 |
| sample_originator | Le, T.X. |
| date_acquired | None |
| Links |
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