Geochemistry Sample Clauses

Geochemistry shall include all analysis performed both on ditch samples and each of the recovered cores.
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Geochemistry. In spite of the fact that most of the gold assays from Whitehouse cannot relied upon, the base metals are perhaps more credible, and some support for a mineral deposit can be seen with Cu, Pb and Zn in stream sediments. Gold in concentrates from soils are also consistently high but no means of quantifying these results could be found, as noted above. 50 He took 21 rock chip and 7 stream sediment samples and all of the latter contained visible free gold as did all 4 taken during this last visit. Copper in rocks was up to 140 ppm with maxima of 20 ppm MO, 385 ppm Pb and 106 ppm Zn also recorded. Up to 1 ppm Au was also found. 51 BIBLIOGRAPHY
Sample 1
Geochemistry. In 1995 and 1996, the Ontario Geological Survey carried out regional till sampling, lake sediment sampling and lake water sampling over an area that included the present XxXxxx property (Bajc, 1996; Bajc et al., 1996). Till samples were collected from 1 m deep pits, and sent for heavy mineral concentration and geochemical analysis. Gold concentration and gold grain information (abundance, size, shape) were used to identify anomalies of potential exploration significance. One of the anomalies identified was the “Xxxxxxx-XxXxxx Trend”, extending from central Xxxxxxx Township east into central XxXxxx Township (Fig. 8). The anomaly was described as “broad, low amplitude”, which “coincides with a structurally-controlled lithologic break between Mg-rich tholeiitic basalts to the north and Fe-rich tholeiitic basalts to the south” (Bajc, 1996). Infill till sampling was recommended to better define the anomaly. Chemical analysis of the matrix to the till produced other interesting data in the northwest part of the XxXxxx property. One till sample had Cu and Ag results in the 98%ile of all the samples, and several minor Zn anomalies are present. The Ontario Geological Survey defined a Au­Ag-Mo±Cu±Ni±Cr±Co till anomaly roughly coincident with the Xxxxxxx-XxXxxx trend in the northwest part of the property (Fig. 8; Bajc et al., 1996). Heavy mineral concentrates from selected till samples collected in 1995/96 were processed to recover Kimberlite Indicator Minerals (KIMs; Bajc and Xxxxxxxx, 2001). This work included the microprobing of 4450 chromite grains; the only grain to plot well within the Diamond Inclusion Field on a binary Cr2O3-MgO diagram was from a till sample taken in the west-central portion of the XxXxxx property, potentially down-ice from the magnetic anomaly shown in Figure 7. No other KIMs were identified from the property, however. The lake sediment and lake water sample density on the XxXxxx property is somewhat less than optimal due to the paucity of lakes. However, even with this constraint, the Ontario Geological Survey managed to define a Sb-As-W-Mo-Ni-Co-Cr-Cu anomaly in the southeast part of the property, coincident with the historical gold mineralization (Fig. 8; Bajc et al., 1996).
Sample 1
Geochemistry. The Lakeview zone had a strong arsenic and gold anomaly. Extensions to the geochenp survey have shown erratic high arsenic, gold and some antimony in other areas deserving follow-up.
Sample 1
Geochemistry. Mitigation Measure WQ-1: If waste rock material from the Mackay North and 5-North pits is not tested, it would not be used as backfill material below the water table and will be treated as potentially acid generating per the WRMP. Only material that has been tested and meets NDEP criteria can be used as backfill below the water table in any of the on-site pits (BLM 2019b).
Sample 1
Geochemistry. Percentile statistics were applied to geochemical values from the humus, "B" and "C" horizon till samples collected from the orientation and regional surveys. Anomalous geochemical values were defined as those which occurred at or above the 95th percentile. Background concentrations were defined as 50th percentile values. These values are summarized for each survey in Tables 4 (gold and base metal) and 5 (rare element pegmatite). Data was plotted as proportional dot diagrams to evaluate element distribution and concentration with respect to bedrock geology. Comparing both 95th and 50th percentile value from orientation surveys with those derived from the regional sampling program highlights several important relationships:
Sample 1

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