The Occurrence of Uranium Ore at Sleisbeck, N.T

- Organization:
- The Australasian Institute of Mining and Metallurgy
- Pages:
- 15
- File Size:
- 1209 KB
- Publication Date:
- Jan 1, 1955
Abstract
Uranium ore at Sleisbeck, N.T., occurs as lenticular bodies associated with zones of bleached carbonized schists lying between walls of closely folded quartzite. The ore consists mainly of uranium micas with Borne pitchblende.INTRODUCTIONThe Sleisbeck uranium prospect is about 70 miles E. of Pine Creek, and 160 miles S.E. of Darwin (Fig. 1). The prospect consists of a well-defined, E.-W. trending line of hills, about I! miles long. The line is composed of 3 major hills called the Eastern, Central and Western hills, with minor interconnecting hills and outcrops (Fig. 2).
Citation
APA: (1955) The Occurrence of Uranium Ore at Sleisbeck, N.T
MLA: The Occurrence of Uranium Ore at Sleisbeck, N.T. The Australasian Institute of Mining and Metallurgy, 1955.