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Collapse features, Temple mountain Uranium area, Utah
Hydrothermal solutions mainly of hypogene origin are believed to be responsible for formation of collapse features, their associated alteration effects, and accompanying mineralization at and near Temple Mountain; collapse features range from less than 100 ft in diam to more than 1000 ft and were formed by removal of underlying carbonate rocks.
Collapse features, Temple mountain Uranium area, Utah
Hydrothermal solutions mainly of hypogene origin are believed to be responsible for formation of collapse features, their associated alteration effects, and accompanying mineralization at and near Temple Mountain; collapse features range from less than 100 ft in diam to more than 1000 ft and were formed by removal of underlying carbonate rocks.
Collapse features, Temple mountain Uranium area, Utah
Geol Soc America -- Bul
Kerr, P.F. (Autor:in) / Bodine, Jr., M.W. (Autor:in) / Kelley, D.R. (Autor:in) / Keys, W.S. (Autor:in)
1957
49 pages
3 Plates
Report
Englisch
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