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LECTURE 10: RADIOMETRIC METHOD
H. Saibi Dec. 11, 2015
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Schematic illustration of the radiometric method
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Exponential decay process
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Interaction of g-rays with matter
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Attenuation of g-rays of different initial energies by various materials encountered in the geological environment.
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Changes in atomic number (Z) and neutron number (N) associated with radioactive decay.
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Energy spectra of g-rays produced by the decay of the 3 main naturally occurring radioelements
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Statistical measurement error versus the number of emission counts recorded
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Examples of modern g-ray spectrometers
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Fields of view
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Factors contributing to the g-ray spectra measured in the field and the corrections applied to reduce the survey data
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Radiometric data presented to highlight only anomalous responses.
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Radioelement content of igneous rocks and selected minerals and ores.
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Radioelement content of metamorphic rocks and selected minerals and ores.
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Radioelement content of sedimentary rocks and selected minerals and ores.
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The 238U decay series showing half-lives and potential mechanisms for disequilibrium within the series
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Schematic illustration of near0-surface processes that affect radiometric responses.
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Abundances of K, U, and Th compared for bedrock and adjacent overburden
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Variations in radioelement concentrations in the soil/regolith profile
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Summary of K and Th concentrations in the vicinity of the Goonumbla-North Parkes Cu-Au porphyry deposits.
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Geochemical data from altered and unaltered rocks from the Waitekauri area
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The Iron King Pb-Zn-Cu-Au-Ag sulphide deposit.
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Schematic illustration of the radiation source areas of various terrain forms for ground radiometric measurements
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Profiles of radiometric data and various channel ratios from the Uranium City area.
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Radiometric data from the Yeelirrie calcrete U deposit.
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Radiometric and magnetic data from the Waihi-Waitekauri epithermal Au-Ag field.
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Data from the Flinders Ranges
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Subsets of the radiometric data
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Examples of g-logs and their relationship to lithology from a range of mineralised geological environments.
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Self-Potential and g-logs through a coal-measured sequence.
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g-logs through iron formations at Jimbledar in the Hamersley iron-ore province of Western Australia.
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