9655605
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU9655605
| Property | Value |
|---|---|
| id | 9655605 |
| igsn | 10.60494/p2bm-vz04 |
| sample_id | NE23/05 |
| eno | 917519 |
| sampling_feature_name | NE23/05 |
| sampling_feature_type | field site |
| sample_type | outcrop specimen |
| sampling_method | outcrop sampling |
| material_class | rock |
| earth_materials | Y |
| stratigraphic_unit | Barrington Tops Supersuite |
| geological_province | New England Orogen |
| sample_remark | Cawood et al 2011 paraphrased: "The Zircons are more elongated with a length to breadth ratio in excess of 5, although most of the extracted grains are broken fragments rather than complete crystals, which most likely results from their unusual elongation. Their internal structures are relatively simple, consisting of either relatively thick oscillatory zones or a simple alteration of even thicker bands of differing CL intensity with no observed dissolution boundaries between zones. |
| 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 | 151.5282418 |
| gda94_latitude | -31.8819927 |
| sample_originator | Cawood, P. |
| date_acquired | 3000-01-01 00:00:00 |
| Links |
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