11086363
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU11086363
| Property | Value |
|---|---|
| id | 11086363 |
| igsn | 10.60494/674c-mm83 |
| sample_id | 75301330 sericite |
| eno | 1041966 |
| sampling_feature_name | MT HOGAN |
| sampling_feature_type | field site |
| sample_type | unknown |
| sampling_method | unknown |
| material_class | rock |
| stratigraphic_unit | Mount Hogan Granite |
| geological_province | None |
| sample_remark | Adjacent to the mineralised quartz lodes. The altered granite mostly consists of about 30% K-feldspar, 40% quartz, 30% secondary fine white mica (presumably sericite) replacing plagioclase, and up to 10% chlorite locally |
| 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 | 143.81699 |
| gda94_latitude | -19.171981 |
| sample_originator | Bain, J. |
| date_acquired | 3000-01-01 00:00:00 |
| Links |
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