Detection of ore deposition stages by multiple correlation method
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Abstract
When searching for deep-seated ore bodies by primary halos usually use two main parameters: zonality and the gradient of element content in primary halos along the upthrust, across and along the strike of ore zones. To study zonality, it is important to assess the stage of ore deposition. Only by assessing the stage of ore deposition, it is possible to study zonality and use it both to search for blind ore bodies, and to assess the level of erosion cut and the prospects of deep horizons of ore bodies that have not been uncovered by erosion.
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References
- Nikitin N. V. Use of vertical zonality of primary halos in estimation of erosional shearing of tin ore bodies of Primorye. Journal of Mining Institute, 1969, vol. LVI, issue 2.
- Grigoryan S.V., Yanishevsky E.M. Endogenous Geochemical Halos of Ore Deposits and Their Use in the Search for Hidden Ore Deposits. Nedra, 1968.
- Malakhov A. S. Correlation coefficient as an indicator of vertical zonality of mineralization in one of the deposits of Kazakhstan. In the collection: Application of Mathematical Methods in Geology. Nauka, Alma-Ata, 1968.
- Burkov Y.K., Borovikov L.I. Correlation analysis of patterns of distribution of small elements for solving questions of sedimentogenesis. International Geol. congress, XXIII session. Reports of Sov. Geologists, Nauka, 1968.
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