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Jasperoid in the United States; its characteristics, origin, and economic significance
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Tridymitic jasperoid deposits in N. W. Queensland
Mineralium Deposita, 1977A number of small, fault-controlled, siliceous, copper deposits in the Precambrian of North-West Queensland contain most of their silica as tridymitic jasperoid. The tridymite has pseudomorphically replaced the dynamic metamorphic assemblages that resulted from earlier fault movements.
W.J. McKay, T. Finlow-Bates
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Mapping of jasperoid in the Cedar Mountains, Utah, U.S.A., using imaging spectrometer data
International Journal of Remote Sensing, 1995Abstract Jasperoid, an important indicator of disseminated gold deposits, is mapped in the Cedar Mountains, Utah U.S.A. using data gathered by the Airborne Visible Infra-Red Imaging Spectrometer (AVIRIS). Ratio analysis is employed to detect the sharp rise in reflectance between 1000 nm and 1700 nm in the jasperoid spectrum due to iron absorption at ...
Richard Murphy
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Jasperoid float and stream cobbles as tools in geochemical exploration for hydrothermal ore deposits
Journal of Geochemical Exploration, 1981Abstract Fragments of silicified rocks that are associated with deposits of base and precious metals may be transported as cobbles and pebbles in alluvium far downstream from the source outcrop. These rocks commonly exhibit certain characteristics which distinguish them from other detrital siliceous material, and may thus serve as a useful tool in ...
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Mineralium Deposita, 2007
Uranium mineralization in the El Erediya area, Egyptian Eastern Desert, has been affected by both high temperature and low temperature fluids. Mineralization is structurally controlled and is associated with jasperoid veins that are hosted by a granitic pluton.
Hamdy Abd El-Naby
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Uranium mineralization in the El Erediya area, Egyptian Eastern Desert, has been affected by both high temperature and low temperature fluids. Mineralization is structurally controlled and is associated with jasperoid veins that are hosted by a granitic pluton.
Hamdy Abd El-Naby
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Chemical Geology, 2009
Abstract The age of the Mesoproterozoic Belt Supergroup hosted silver and base metal vein deposits of the Coeur d'Alene mining district in northern Idaho has long been controversial. Evidence for Precambrian mineralization comes largely from many ∼ 1400 Ma Pb model ages for galena throughout the district, and several problematic 1100–1300 Ma 207Pb ...
Joseph V Smith, Robert E Zartman
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Abstract The age of the Mesoproterozoic Belt Supergroup hosted silver and base metal vein deposits of the Coeur d'Alene mining district in northern Idaho has long been controversial. Evidence for Precambrian mineralization comes largely from many ∼ 1400 Ma Pb model ages for galena throughout the district, and several problematic 1100–1300 Ma 207Pb ...
Joseph V Smith, Robert E Zartman
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Micron Gold-Associated Jasperoid: Fluid Inclusion Chemistry and Geothermometry
Journal of Geochemical Exploration, 1986Patricia H. Schnorr +2 more
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