Comparison of Secondary Fe-Mn Oxides in Fracture Coatings and Heavy-Mineral Concentrates as Sampling Media, Silver City Mining Region, New Mexico

The American Institute of Mining, Metallurgical, and Petroleum Engineers
K. C. Watts University of Georgia T. T. Chao J. R. Hassemer R. F. Sanzolone
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
8
File Size:
557 KB
Publication Date:
Jan 1, 1984

Abstract

Secondary oxides of Fe-Mn have been used in mineral exploration from the time gossans were first recognized Since gossans are conspicuous features and are largely explored, it is necessary to look for more subtle indication of blind mineralization. Sampling materials used in these geochemical studies consist of secondary Fe-Mn oxide-rich products of hydrothermal mineralization, and "in situ" weathering found in fracture fillings-as selvages along joints and disseminations in host rock. These materials were selectively collected and studied in the Silver City mining region. Two independent sampling methods were compared. The difference in the sampling methods was mainly in the ways samples were obtained and processed. One method involved systematic sampling of fracture fillings and coatings from which secondary Fe and Mn oxides and associated trace elements were then selectively extracted by chemical methods. The second approach involved collection of composite stream sediments and physical extraction of Fe-Mn oxide materials by gold panning, bromoform concentration, and electromagnetic separation. The source of the Fe-Mn-rich materials in the stream sediments is considered to be fracture fillings and coatings that mechanically entered the drainage basins. Map distributions of the two-sample types were compared. Both methods showed generally supportive patterns of anomalous metal dispersion, although anomaly-to-background contrast seems better in joint coatings. Both were useful in distinguishing geochemical differences between mining districts in the region. For example, the Pinos Altos district may contain more hydrothermally-introduced iron than the Central district, whereas the Central district has lead and zinc enrichments that are less on the amount of iron enrichment than is the case in the Pinos Altos district. The methods were qualitatively compared relative to time, expense, and other advantages and disadvantages.
Citation

APA: K. C. Watts University of Georgia T. T. Chao J. R. Hassemer R. F. Sanzolone  (1984)  Comparison of Secondary Fe-Mn Oxides in Fracture Coatings and Heavy-Mineral Concentrates as Sampling Media, Silver City Mining Region, New Mexico

MLA: K. C. Watts University of Georgia T. T. Chao J. R. Hassemer R. F. Sanzolone Comparison of Secondary Fe-Mn Oxides in Fracture Coatings and Heavy-Mineral Concentrates as Sampling Media, Silver City Mining Region, New Mexico. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1984.

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