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These were not determined. Table 8 of Hackman et al. (1989) is reproduced below to show the differences between the analyses produced by the two laboratories. In the geochemistry database, absent data is recorded as a blank in character fields and as -1 in numeric fields.
Table 8: Threshold (upper) and background (lower) levels in relation to drainage basin lithology groups (see Explanation of field codes for explanation of letter codes).
| Zn | Pb | Ni | Co | Mn | Cu | Sr | Ba | Li | |
|---|---|---|---|---|---|---|---|---|---|
| QG | 15041 | 201 | 5014 | 4012 | 3000468 | 8018 | 15532 | 500118 | 195 |
| OB | 10045 | 161 | 7017 | 5015 | 1200438 | 6023 | -33 | -132 | -5 |
| X | 8035 | 102 | 3513 | 2712 | 1500510 | 5017 | 15030 | 240114 | -5 |
| SK | 17037 | 201 | 60020 | -14 | 3000384 | 20025 | 25046 | 500132 | -5 |
| MBU | 10038 | -1 | 100021 | -17 | 2000453 | 17023 | 25036 | -130 | -5 |
| KL | 15044 | 202 | 7015 | 3512 | 1600476 | 4515 | 25039 | 350107 | 226 |
| MKV | 14557 | 2513 | 8029 | 5224 | 50001190 | 4017 | 400121 | 300130 | 205 |
| N | 15582 | 3518 | 11037 | 10039 | 70002247 | 6529 | 100093 | 450213 | 152 |
| Zn | Pb | Ni | Co | Mn | Cu | Sr | Ba | Li | |
|---|---|---|---|---|---|---|---|---|---|
| D | 20030 | 3010 | 10021 | 5016 | 2500555 | 4013 | 60071 | 30086 | 302 |
| LM | 8026 | 307 | 5016 | 309 | 1100295 | 308 | 35074 | 20055 | 122 |
| M | 8035 | 2110 | 3518 | 2816 | 2000629 | 3013 | 20059 | 20588 | 264 |
| P | 10046 | 4017 | 10027 | 2616 | 30001257 | 2512 | 35075 | 300135 | 102 |
| SO | 12052 | 3012 | 5025 | 5120 | 4000972 | -16 | 700110 | 400132 | 203 |
| Zn | Pb | Ni | Co | Mn | Cu | Sr | Ba | Li | |
|---|---|---|---|---|---|---|---|---|---|
| D | 11041 | 401 | 6015 | 3514 | 2000427 | -17 | 15027 | 400103 | -3 |
| LM | 14041 | 203 | 4216 | 2712 | -528 | 4515 | 20049 | 400126 | -6 |
| M | 12542 | 201 | 4015 | 7013 | -422 | 5519 | 13530 | 350103 | 305 |
| P | 20069 | 404 | 4010 | 5014 | 50001184 | -13 | 16031 | 500161 | -7 |
| SO | 20062 | 152 | 7014 | 7016 | -752 | 6017 | 19063 | 500181 | -7 |