Property Value
id 9655247
igsn 10.60494/4c64-je43
sample_id Wilyerpa Formation
eno 912542
sampling_feature_name Wilyerpa Formation
sampling_feature_type field site
sample_type outcrop specimen
sampling_method outcrop sampling
material_class rock
stratigraphic_unit Wilyerpa Formation
geological_province Stuart Shelf
sample_remark Fanning & Link (2008): In general terms, Sturtian sections across South Australia contain a series of diamictite layers that have interbedded silts (e.g. Link and Gostin, 1981) and these have highly prospective layers that we consider to be tuffaceous or volcaniclastic in origin. West of Copley in northern South Australia, a tuffaceous bed in the lower Wilyerpa Formation, Yudnamutana Subgroup, Umberatana Group has a dominant igneous age component at ca. 659 Ma. This tuffaceous horizon is within the Wilyerpa Formation that comprises heterogeneous bedded diamictite, sandstone and siltstone containing ice-rafted debris, across the central and northern Flinders Ranges. At Copley, dropstones are abundant in the Wilyerpa Formation above and below the tuff bed. This 659 Ma age constraint on the Sturtian glaciation is consistent with Re-Os ages on post-Sturtian glacial black shales from Tindelpina Member of Tapley Hill Formation South Australia (643 +/- 2.4 Ma; Kendall et al. 2006) and Aralka Formation, Central Australia (657.2 +/- 5.4 Ma).
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 EFTF - Isotopic Atlas of Australia
gda94_longitude 138.3901389
gda94_latitude -30.5596944
sample_originator Fanning, C.M.
date_acquired 2000-01-01 00:00:00
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