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This secondary mineralization has been derived from decomposition and leaching of the primary mineralized zone, and forms a tongue-like fan of ore-grade material dispersed down-slope for about 80 m to the south-east.
This paper was originally published in the Proceedings of the Third International Conference on Creationism, pp.
497–504 (1994) and is reproduced here with the permission of the Creation Science Fellowship of Pittsburgh.
Owing to the isoclinal recumbent folding of metasedimentary units of the Cahill Formation, the typical rock sequence encountered at Koongarra is probably a tectono-stratigraphy (from youngest to oldest.) foliation of the schist sequence, which at Koongarra dips at 55° to the south-east.
The dominant structural feature, however, is the reverse fault system that dips at about 60° to the south-east, sub-parallel to the dominant S foliation and lithological boundaries, just below the mineralized zone.
A thick sequence of essentially flat-lying sandstones (the Middle Proterozoic Kombolgie Formation) was then deposited unconformably on the Archean- Lower Proterozoic basement and metasediments.
At Koongarra subsequent reverse faulting has juxtaposed the lower Cahill Formation schists and Kombolgie Formation sandstone.
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The Koongarra uranium deposit occurs in a metamorphic terrain that has an Archean basement consisting of domes of granitoids and granitic gneisses (the Nanambu Complex), the nearest outcrop being 5 km to the north.Tags: Adult Dating, affair dating, sex dating