best magazine for ias preparation
best magazine for ias preparation
Wyomings Geology Potential for U.S. Utilities
best magazine for ias preparation Boberg explained the development of the roll-fronts, writing,
“Fluid flow through the very porous and permeable sediments would be relatively
fast allowing for the development of large oxidized tongues with the young
sediment as well as scattered uranium deposits at the redox (oxidized
reduction) interface within approximately a million years. Deposits formed near
the granitic highlands would be larger and of higher average grade because of
the proximity to the dual source of granite and ash. pratiyogita darpan pdf ” J.D. Loves uranium discovery in Tertiary
sandstones, in 1951, was a near-surface roll-front type of redox deposit. A
roll-front deposit follows a sinuous linear trend, often C-shaped. Colorado and
Utah miners began calling the cross-sectional configuration a “roll” in the
early 1940s. Roll-fronts occur in sandstones, bordered above and below by less
permeable shales. pratiyogita darpan in hindi In Wyoming, the “rolls” are
bordered by altered and unaltered sandstone. It is generally concave from
altered ground and convex into unaltered ground. Harris idealized roll-front
uranium deposit would have “uranium concentrations decrease abruptly away from
the concave boundary, and concentrations gradually decrease away from the
convex boundary in reduced rock.” Uranium is not always present everywhere
along a roll front. pratiyogita darpan online It may be unevenly distributed and there are
often other elements, such as vanadium, selenium, molybdenum, copper, silver,
lead and zinc. Geologists look for where coarse-grained sandstones grade into
finer grained or clay-bearing equivalents as indicators for uranium ore. As
uranium geologists know with roll-front deposits, it may be mined as long as it
is below the water table. Once deposits are brought above the water table, the
uranium concentration can be eroded and severely modified pratiyogita darpan yearbook 2016 .

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