Detecting Mineralization Using Partial Element Extractions: A Case Study
نویسنده
چکیده
Detecting deep mineralization from partial element concentrations in surface and near-surface samples requires detecting the signature of one geochemical process against a background that arises from many other geochemical processes. Since the last glaciation of the Canadian Shield, it is believed that only H+ can have diffused through substantial overburden, and hence that the only available signatures for underlying mineralization must be based, directly or indirectly, on pH. We show that direct observation of pH may not be a reliable signature for underlying mineralization, but that signatures based on the indirect effects of a pH low are readily visible using matrix decompositions.
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تاریخ انتشار 2004