Publication Laka-library:
Uranium in the Pine Creek Geosyncline (1980)
| Author | IAEA |
| Date | 1980 |
| Classification | 4.22.5.12/01 (AUSTRALIA - MINES - JABILUKA) |
| Front |
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From the publication:
FOREWORD The International Uranium Symposium on the Pine Creek Geosyncline was designed to present original data and interpretations of the Geosyncline derived from a three year coordination study by the sponsoring organisations: Bureau of Mineral Resources, Geology and Geophysics (BMR); Commonwealth Scientific and Industrial Research Organisation, Institute of Earth Resources (CSIRO) and participating industry groups. Papers contained in this volume were presented at the Symposium held in Sydney, Australia, June 4-8, 1979. The sponsoring organisations wish to express their gratitude to the International Atomic Energy Agency (IAEA) for its co-operation in the Symposium and the publication. Uranium exploration in the Pine Creek Geosyncline was stimulated by the discovery in 1949 of secondary uranium mineralization near Rum Jungle by the prospector J.M. White. This was followed by a decade of intense exploration activity resulting in the discoveries of uranium at Rum Jungle and in the South Alligator Valley. The first systematic mapping survey of the region also commenced during this period. The potential similarity of the Alligator Rivers area to the Rum Jungle Uranium Field was shown by a re-interpretation of the geology as shown on the second edition of the 1:500 000 scale map of the Geosyncline (Walpole et al., Bull. Bur. Miner. Resour. Geol. Geophys., Aust., 82, 1968). All the major uranium deposits of the Alligator Rivers Uranium Field have been discovered since 1970. The present resources (RAR) of the Geosyncline are approximately 289,000 tonnes U30s, more than 15 percent of the Western World's uranium resources. The papers contained in this volume deal with regional and detailed aspects of exploration, geophysics, stratigraphy, geochemistry and petrology. In addition to the coverage of many aspects of uranium distribution and mineralization within the Pine Creek Geosyncline, vein-type uranium deposits in Lower Proterozoic rocks in other countries are discussed and compared with the Australian deposits. Particular emphasis is given to the Athabasca margin deposits in Canada. A pleasing aspect of the Symposium was the diverse range of hypotheses advanced to account for the 'unconformity type' uranium deposits. It became clear that workers on the Canadian Athabasca margin deposits put much more emphasis on the genetic role of the unconformably deposited Middle Proterozoic rocks than do the Australian workers. Although the Symposium acted as a landmark in the progress towards an understanding of the uranium mineralization in the Pine Creek Geosyncline, it is natural to expect that further studies will confirm or modify some of the concepts put forward here.
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