6661373
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU6661373
| Property | Value |
|---|---|
| id | 6661373 |
| igsn | 10273/AU6661373 |
| sample_id | ERNEST HENRY |
| eno | 649134 |
| sampling_feature_name | CLONCURRY_ERNEST HENRY |
| sampling_feature_type | field site |
| sample_type | outcrop specimen |
| sampling_method | outcrop sampling |
| material_class | rock |
| earth_materials | Y |
| stratigraphic_unit | Mount Fort Constantine Volcanics |
| geological_province | Carpentaria Lowlands Region |
| sample_remark | Mark et al 2006: "The Ernest Henry hydrothermal system was formed by two cycles of sodic and potassic alteration where biotite–magnetite alteration produced in the first cycle formed ca 1514+/-24 Ma, whereas paragenetically later Na–Ca veining formed ca 1529 +11/-8 Ma. These new U-Pb titanate age dates support textural evidence for incursion of hydrothermal fluids after the metamorphic peak, and overlap with earlier estimates for the timing of Cu-Au mineralization (ca 1540–1500 Ma)." |
| 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 | None |
| mineral_deposit_waste_samples | None |
| linked_files | None |
| other_geological_data | None |
| project_name | None |
| gda94_longitude | 140.7052056 |
| gda94_latitude | -20.4430861 |
| sample_originator | Jones, S. |
| date_acquired | 2000-01-01 00:00:00 |
| Links |
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