Possibility of reducing the time of spectrum photographing when analyzing metallometric samples
Abstract
A number of geological questions are solved using spectral analysis data. Spectral analysis also acquires practical importance in geochemical studies, in particular, in metallometric survey. In combination with geophysical methods in parties and expeditions in search and study of scattering halos of various chemical elements, a large number of analyses for lead, molybdenum, tin, copper, zinc, tungsten, antimony, nickel, cobalt, arsenic and other elements are performed. In this case, spectral determinations of metals are made in samples of loose sediments (sediment). When searching for ore bodies that do not extend below the sediment, disseminated mineralization at some distance from the ore bodies can also be detected by spectral sampling of bedrock or sediment from the surface.
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