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Economic Geology GSW 2008 Users' Group Meeting
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Economic Geology; June 1956; v. 51; no. 4; p. 354-361
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Notes on the geotectonics and uranium mineralization in the northern part of the Northern Territory, Australia

J. Rade

Notes the association of uranium mineralization in the Katherine-Darwin region, Northern Territory, with zones of shattered rock formed by shearing along anticlines and horizontal displacement along northeast-trending faults. These structures are thought to have originated as a result of dislocation of crustal blocks, which was caused by deep-seated subcrustal flow (bathyrheal underflow) in a northeasterly direction.

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