2171003
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU2171003
| Property | Value |
|---|---|
| id | 2171003 |
| igsn | 10273/AU2171003 |
| sample_id | 2004089520A |
| eno | 576014 |
| sampling_feature_name | KLD103 |
| sampling_feature_type | borehole |
| sample_type | core |
| sampling_method | core diamond |
| material_class | rock |
| stratigraphic_unit | Tin Camp Granite |
| geological_province | Pine Creek Orogen |
| sample_remark | The Tin Camp Granite is a pervasively altered biotite granite, which intrudes Nimbuwah Complex granodioritic migmatites, is faulted against the Oenpelli Dolerite, and is unconformably overlain by the Kombolgie Subgroup in the eastern Pine Creek Orogen (Needham 1988). The constituent minerals are quartz-plagioclase-K-feldspar-biotite, although the feldspars and biotite are altered to sericite and chlorite respectively. |
| earth_materials | Y |
| structural_measurements | None |
| inorganic_geochemistry | Y |
| organic_geochemistry | None |
| geochronology | Y |
| isotope_groups | Y |
| hydrochemistry | None |
| rock_properties | None |
| mineralogy | None |
| thin_sections | None |
| repository_samples | Y |
| mineral_deposit_samples | None |
| mineral_deposit_waste_samples | None |
| linked_files | None |
| other_geological_data | None |
| project_name | None |
| gda94_longitude | 133.4270188 |
| gda94_latitude | -12.4890834 |
| sample_originator | Worden, K.E. |
| date_acquired | None |
| Links |
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