1925609
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU1925609
| Property | Value |
|---|---|
| id | 1925609 |
| igsn | 10273/AU1925609 |
| sample_id | 2005670100 |
| eno | 408092 |
| sampling_feature_name | 2005670100 |
| sampling_feature_type | field site |
| sample_type | outcrop specimen |
| sampling_method | outcrop sampling |
| material_class | rock |
| stratigraphic_unit | Talbot schist |
| geological_province | Rudall Province |
| sample_remark | Quartz-K-feldspar-muscovite schist was sampled from the northwestern part of the Talbot Zone (MGA 401083E 7507460N), where unassigned metasedimentary schist occurs adjacent to layered granite orthogneiss. Hickman and Bagas (1999) suggested that these metasedimentary rocks might pre-date layered orthogneiss and thus comprise some of the oldest rocks in the Talbot Zone. The sampled schist contains a high-grade layer-parallel foliation containing medium- to coarse-grained muscovite, which is folded about mesoscale tight, upright, northwesterly trending F4 folds. The schist forms part of a compositionally layered succession defined by differing abundances of quartz, muscovite and feldspar. In thin section, the schist consists of thin interlayered domains of granoblastic medium-grained quartz, microcline and lesser plagioclase, bound by laminae of layer-parallel muscovite, which comprises up to 15% of the rock. |
| 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 | 122.0380709 |
| gda94_latitude | -22.5365919 |
| sample_originator | Maidment, D.W. |
| date_acquired | None |
| Links |
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