2 edition of Origin and modification of a uraninite-bearing placer, Elliot Lake, Ontario. found in the catalog.
Origin and modification of a uraninite-bearing placer, Elliot Lake, Ontario.
Written in English
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Evidence of detrital forms in the gold has confirmed its placer origin prior to modification during metamorphism. Furthermore, rhenium-depletion ages ranging from to Ga for Witwatersrand gold support numerous other lines of evidence that have been used in the past to interpret the gold, uranium and pyrite concentrates as Archean placers.
Derry D R, - Evidence of the origin of the Blind River uranium deposits: in Econ. Geol. v pp. ; Robinson A, Spooner E T C - Postdepositional modification of Uraninite-bearing quartz-pebble conglomerates from the Quirke Ore Zone, Elliot Lake, Ontario: in Econ.
Geol. v79 pp Robinson A, Spooner ETC () Postdepositional modification of uraninite-bearing quartz-pebble conglomerates from the Quirke Ore Zone, Elliot Lake, Ontario.
Econ Geol – Google Scholar Ronov AB () Common evolutionary trends in the chemical composition of sedimentary and igneous rocks of the Earth’s by: 1. Robinson A, Spooner E T C - Postdepositional modification of Uraninite-bearing quartz-pebble conglomerates from the Quirke Ore Zone, Elliot Lake, Ontario; in Econ.
Geol. v79 pp Samson I M - Fluid evolution and mineralization in a subvolcanic granite stock: The Mount Pleasant W-Mo-Sn deposits, New Brunswick, Canada; in Econ. Adequate services, expertise and modern technologies are needed to ensure a sustainable supply of uranium raw materials to fuel both operating and future nuclear power reactors.
Effective regulation, sound environmental management, training and education are required to minimize the impact of uranium mining and production and to contribute to public acceptance of the global. Full text of "Systematic mineralogy of uranium and thorium" See other formats.
The best depth of the lake is 36m\, and pH value of t he water is \, whose mineralization degree of is g/L.\n\nUran ium concentrations of the salt lake are around ~ μg/L and the avera ge value is μg/L.
Uranium concentrations near the shores are higher t han that of being river supplies and the deep higher than the upper. Principles of Precambrian Geology represents an updated abridgment of my book Precambrian Geology: The Dynamic Evolution of the Continental Crust.
The new book covers the same ground and reaches the same broad conclusions as its parent, but in reduced, less densely illustrated format. developments in sedimentology 41 diagenesis, i further titles in this series volumes i, and are out of print 12 r.c.g.
bathurst carbonate sediments and their diagenesis 16 h.h. rleke iii and g. chilingarian compaction of argillaceous sediments 17 m.d. picard and l.r. high jr. sedimentary structures of ephemeral streams 18 g.
chilingarian and k.h. wolf, editors .