9655743
Persistent Identifier: https://pid.geoscience.gov.au/sample/AU9655743
| Property | Value |
|---|---|
| id | 9655743 |
| igsn | 10.60494/cspc-eh91 |
| sample_id | KDD |
| eno | 917465 |
| sampling_feature_name | KDD |
| sampling_feature_type | field site |
| sample_type | outcrop specimen |
| sampling_method | outcrop sampling |
| material_class | rock |
| stratigraphic_unit | Kadoona Dacite Member |
| geological_province | Lachlan Orogen |
| sample_remark | Kemp et al 2007 paraphrased: "The I-type Kadoona Dacite (Wyborn & Chappell 1986) is an ignimbrite unit of 40 km strike length that outcrops near the northern extremity of the Glenbog Suite.The sample is a massive brownish grey, strikingly crystal-rich rock containing abundant plagioclase, strongly embayed quartz, augite and orthopyroxene phenocrysts in a devitrified groundmass mosaic with a barely discernible eutaxitic fabric. Zircons are sparsely scattered through the groundmass, and form rare inclusions in plagioclase and pyroxene crystals. Zircon inclusions also occur in phenocrysts of the other volcanic rocks examined herein. The Kadoona Dacite and Glenbog Granodiorite are regarded as the type example of a consanguineous I-type volcano-plutonic association (Wyborn & Chappell 1986; Chappell et al. 1987)." |
| earth_materials | Y |
| 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 | 149.648808 |
| gda94_latitude | -35.748908 |
| sample_originator | Kemp, A. |
| date_acquired | 3000-01-01 00:00:00 |
| Links |
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