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
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