9655541
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU9655541
| Property | Value |
|---|---|
| id | 9655541 |
| igsn | 10.60494/6g6t-d433 |
| sample_id | KB16 |
| eno | 917452 |
| sampling_feature_name | KB16 |
| sampling_feature_type | field site |
| sample_type | outcrop specimen |
| sampling_method | outcrop sampling |
| material_class | rock |
| earth_materials | Y |
| stratigraphic_unit | Noonthorangee Formation |
| geological_province | Delamerian Orogen |
| sample_remark | Johnson et al 2016 paraphrased: "The sample was collected fromthe Noonthorangee Formation of the Ponto Group, which is located in the hangingwall of the Koonenberry Fault. Quartz is the dominant mineral in this sample, with minor abundances of detrital muscovite, plagioclase and alkali feldspar. Quartz grains are characterised by the development of subgrain boundaries, which reflects the higher-grade of metamorphism and strain attained by these rocks. Oscillatory zoning is dominant in the majority of the detrital zircon grains extracted from this sample." |
| 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 | 142.3966111 |
| gda94_latitude | -30.6286667 |
| sample_originator | Johnson, E. |
| date_acquired | 3000-01-01 00:00:00 |
| Links |
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