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2019-10-10_HYDROLOGY - M1980244 (22)
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2019-10-10_HYDROLOGY - M1980244 (22)
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Last modified
1/18/2025 6:46:01 AM
Creation date
10/15/2019 3:42:22 PM
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Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
HYDROLOGY
Doc Date
10/10/2019
Doc Name Note
Waste Rock Geochemical Characterization Study Report
Doc Name
Vol. II, Part 2 of 2
From
CC&V
To
DRMS
Email Name
TC1
Media Type
D
Archive
No
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IIII I HRl I Iijini I I 1*11 19 U11 is to cl, <br /> r- <br /> -41 <br /> CO TA <br /> L <br /> OD <br /> 0) WE <br /> OD Samples Recommended for Phase 11 Testing AS <br /> C) Denver. Irc. <br /> C) <br /> ill, a <br /> ton <br /> AP7 No measurable pyrite content. Mid NNP range of ANP. <br /> 82 Neutralizing breccia high end of NNP range. Has 6%dolomite and 3%pyrite.Also contains other <br /> carbonate minerals that may not provide neutralization capacity under environmental conditions. <br /> B3 Sulfidic breccia.Has 2%pyrite,siderite, rhodochrosite. High end of NNP range,but these carbonate <br /> minerals may not provide effective neutralization. <br /> B5 Mid range of NNP.Moderate pyrite content.Contains calcian siderite,which may not provide effective <br /> neutralization. <br /> 67 Sulficlic breccia.with 7%pyrite and 2%calcian siderite. Low end of NNP range.Calcian siderite may not <br /> provide effective neutralization. <br /> 88 Oxidized breccia.Has alunite pyrolusite. hematite.and goethite but no pyrite. <br /> 812 Near zero NNP value,uncertainty with respect to net neutralizing ability under environmental <br /> conditions.Sample with low pyrite content. <br /> L2 The only lamprophyre sample available, <br /> PO The only Precambrian sample.The only sample containing the phlogopite mineral.Average NNP, <br /> PIP2 Upper range of measured NNP values and does not have any measurable pyrite. <br /> PP4 Mid range of NNP and does not have any measurable pyrite content. <br /> Lowest NNP of samples recommended for further analysis. Does not contain carbonate minerals but <br /> PP6 does contain silicate minerals. <br /> cQ <br /> CD <br /> 0 <br /> h <br />
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