Property Value
id 7935615
igsn 10273/AU7935615
sample_id CAB1
eno 816986
sampling_feature_name CAB1
sampling_feature_type field site
sample_type outcrop specimen
sampling_method outcrop sampling
material_class rock
earth_materials Y
stratigraphic_unit Parmeener Supergroup
geological_province Tasmania Basin
sample_remark Bacon & Green (1984) paraphrased: "Airfall tuff occurs as a very minor component in a sedimentary sequence comprised dominantly of lithic sandstone interbedded with mudstone, siltstone and thin coal seams. The sedimentary sequence has been extensively intruded by Jurassic dolerite, the dolerite now capping the plateau country of the central Eastern Highlands. The area has also been disrupted by faulting of probable Tertiary age. The sample dated contains... biotite, occurring as fresh flakes up to approximately 30 x 100 ~m in size, and aligned in such a way as to suggest compaction of the airfall tuff."
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 EFTF - Isotopic Atlas of Australia
gda94_longitude 148.222411
gda94_latitude -41.8263277
sample_originator Waltenberg, K.
date_acquired 2000-01-01 00:00:00
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