2130080
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU2130080
| Property | Value |
|---|---|
| id | 2130080 |
| igsn | 10273/AU2130080 |
| sample_id | TH438 |
| eno | 11424 |
| sampling_feature_name | GSQ Mitchell 1 |
| sampling_feature_type | borehole |
| sample_type | core |
| sampling_method | core diamond |
| material_class | rock |
| earth_materials | Y |
| stratigraphic_unit | None |
| geological_province | Thomson Orogen |
| sample_remark | GSQ Mitchell 1 was drilled in 1972 by the Geological Survey of Queensland. It intersected high-grade metasedimentary rocks of the Nebine Ridge at 717.9 metres after penetrating sediments of the Surat Basin (Wallin, 1974). The metasedimentary units in Mitchell 1 consist of interbedded metasiltstone, metasandstone and quartzite. The basement lithologies are phyllitic to schistose and generally steeply dipping with s0 parallel to s1. Sample 2130080/TH438 from 767.49-770.53 metres consists of laminated quartz-mica phyllite. In thin section the rock is characterised by alternating quartz-rich and phyllosilicate-rich layers. Quartz is highly strained and recrystallised. Phyllosilicate-rich layers include varying proportions of quartz and exhibit anastomosing shear zones. Detrital grains include quartz, muscovite (identified as larger grains within phyllosilicate-rich layers) and rare feldspar. |
| structural_measurements | None |
| inorganic_geochemistry | Y |
| organic_geochemistry | None |
| geochronology | Y |
| isotope_groups | None |
| 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 | 147.116667 |
| gda94_latitude | -26.416667 |
| sample_originator | Cross, A.J. |
| date_acquired | None |
| Links |
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