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ANOMALY/BACKGROUND SEPARATION BY APPLYING THE CORRESPONDENCE ANALYSIS METHOD IN THE ENJERD SKARN, IRAN

A. Hezarkhani, S. Bagherifar

First published: 2006DOI pendingView metrics

Abstract

The Correspondence Analysis Method (CAM) is actually a Non-structural method that could be used to define the anomaly from the background. To apply this method, representative samples of a large area are necessary but knowing the exact location of each sample is not necessary. Base on this method, the litho-geochemical data would be mathematically process to extract the valuable factors needed to plot a two by two diagram. This method has been applied on available data in Enjerd skarn deposit. Five factors have been calculated by applying this method, which is resulted to a 5 columns final matrix. According to these factors, we could plot variety diagrams, resulting to; the samples No. 21, 28, 19 and 23 for Cu, No. 4, for Zn, No. 22 for Pb, No. 26, 29 and 30 for Co and Ni, show actual anomalies, respectively. In most diagrams Co and Ni are Para genetically related, since they show very clear Co-separation features.

Publication details

Title
ANOMALY/BACKGROUND SEPARATION BY APPLYING THE CORRESPONDENCE ANALYSIS METHOD IN THE ENJERD SKARN, IRAN
Authors
A. Hezarkhani, S. Bagherifar
Proceedings
6th International Scientific Conference - SGEM
Publisher
SGEM Scientific GeoConference
Year
2006
Pages
193-204
ISSN
1314-2704
ISBN
954-918181-2
Language
en
Publication type
Conference Paper
Keywords
References17
  1. Berberian, M., (1976), Contribution of the Seismotectonics of Iran (Part ІІ). Geological Survey of Iran. V. 39, p518

  2. Berberian, M., (1983), The Southern Caspian: A Compressional depression floored by a trapped, modified oceanic crust: Canadianjournal of Eart Sciences. V. 20, p.163 -183

  3. Mehrpartou, M., (1993). Contribution to the geology, geochemistry, ore genesis and fluid inclusion investigations on sungon Cu-Mo porphyry deposit, (North -West of iran), Ph.D thesis, Hamburg Univ. Hamburg, p. 245.

  4. Stocklin, J., (1977), Structural Correlation of the alpine ranges between Iran and Center Asia. Mem. H. Aser. Society of Geologique France, p333 -353.

  5. Berberian, M., and King, G. C. (1981), Toward a Pale-geography and tectonic evolution of Iran: Canadian Journal of Earth Sciences. V. 18, p. 210-265.

  6. Hongjin, J., Youngzheng, Z., and Xisheng, W., (1995), Correspondence Cluster Analysis and its application in Exploration Geochemistry, Journal of Geochemistry

  7. Exploration, V.55, P. 137-144.

  8. Valenchon, F. (1982), The Use of Correspondence Analysis in geochemistry, Mathematical Geology, V.14 (4), p. 331-342.

  9. Hasanipak, A. and Sharafodin, M. (2002), Exploration Data analysis, Tehran university publication.

  10. Hezarkhani, A. (2003), Anjerd Skarn Geochemistry and its Association with Economic Copper Mineralization, Azarbaijan - Iran, Journal of Amirkabir university, p.158 -175. 6th International Multidisciplinary Scientific GeoConference SGEM2006 www.sgem.org Int er nat ional Confer ence SGEM 200 6 12

  11. Yardley, B. W. D., Rochelle, C. A., Barnicoat, A. C., and Lloyd, G. E., 1991, Oscillatory zoning in metamorphic minerals: an indicator of infiltration metasomatism: Mineralogical Magazine, v. 55,. p. 357-365.

  12. Jamtveit, B, 1991, Oscillatory zonation patterns in hydrothermal grossular- andradite garnet: nonlinear dynamics in regions of immiscibility. American Mineralogist, v. 76, p. 1319-1327.

  13. Jamtveit, B., Bucher-Nurminen, K., and Stijfhoorn, D. E., 1992, Contact metamorphism of layered shale-carbonate sequence in the Oslo Rift: I. Buffering, infiltration and the mechanisms of mass transport: Journal of Petrology, v. 33, p. 327-422.

  14. Kwak, T. A. P., and Tan, T. H., 1981, The geochemistry of zoning in skarn minerals at the King Island (Dolphin) Mine: Economic Geology, v. 76, p. 468-497.

  15. Crawford, M. L., 1977, Calcium zoning in almandine garnet, Wissahickon formation, Philadelphia, Pennsylvania: Canadian Mineralogist, v. 15, p. 243-249.

  16. Einaudi, M. T., 1977, Petrogenesis of the copper-bearing skarn at the Mason Valley mine, Yerington district, Nevada: Economic Geology, v. 72, p. 769-795.

  17. Hezarkhani, A., and Williams-Jones, A. E., 1998, Controls of alteration and mineralization in the Sungun porphyry copper deposit: Evidence from Fluid Inclusion and Stable Isotopes. Economic Geology, v. 93, p. 651-670. 6th International Multidisciplinary Scientific GeoConference SGEM2006 www.sgem.org

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