
Postscript.
Since this paper went to the press, an example of the North Range rocks termed “tuffaceous greywacke” on pp. 83, 85 (e.g., 8932) has been figured by Williams, H., Turner, F. J., and Gilbert, C. M. (1954) in their new book Petrography, as fig. 99c, p. 303, under the classification of “volcanic greywacke”. Except in those cases where a contemporaneous pyroclastic admixture can be proved, as for example by the presence of glass shards, this name is to be preferred to the term “tuffaceous greywacke” as used on the above mentioned pages. Some of the Upper Triassic sediments such as 8952, p. 90, can also be classified appropriately as volcanic greywackes.

[The section below cannot be correctly rendered as it contains complex formatting. See the image of the page for a more accurate rendering.]
| Ionic Radius | Limit of Sensitivity | 8871 | 8873 | 8932 | 8776 | 8768 | 8791 | 8800 | 8859 | 8829 | 8819 | 8817 | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ga | 0.62 Å | 5 | 20 | 20 | 20 | 15 | 10 | 8 | 20 | 15 | 10 | X | 5 | Ga |
| Ci | 0.64 | 1 | 30 | 25 | 80 | X | 7 | 8 | 10 | 3 | n.d. | tr.? | n.d. | Cr |
| V | 0.65 | 10 | 100 | 125 | 250 | X | 20 | 20 | 35 | 20 | n.d. | 20 | n.d. | V |
| Li | 0.78 | 1 | 60 | 55 | 35 | 25 | 45 | 20 | 30 | 30 | 30 | 60 | 80 | Li |
| Ni | 0.78 | 2 | 10 | 10 | 30 | X | X | X | X | X | n.d. | X | n.d. | Ni |
| Co | 0.82 | 5 | 20 | 15 | 30 | X | X | X | X | X | n.d. | X | n.d. | Co |
| Sc | 0.83 | 10 | 20 | X | 25 | X | 10 | X | 20 | X | n.d. | X | n.d. | Sc |
| Zr | 0.89 | 10 | 165 | 100 | 200 | 150 | 175 | 160 | 275 | 150 | n.d. | 175 | n.d. | Zr |
| Cu | 0.83 | 5 | 25 | 40 | 25 | X | 10 | 5 | 10 | 15 | n.d. | 10 | n.d. | Cu |
| Y | 1.06 | 15 | 30 | 30 | 40 | X | 35 | 35 | 45 | 35 | n.d. | 30 | n.d. | Y |
| Sr | 1.27 | 10 | 2,000 | 50 | 200 | 3,500 | 5,000 | 40 | 100 | 10 | 20 | 25 | 15 | Sr |
| Pb | 1.32 | 15 | tr. | X | X | X | 15 | 20 | 25 | 20 | 10 | 10 | 10 | Pb |
| Ba | 1.43 | 10 | 500 | 40 | 200 | 3,000 | 2,000 | 10 | 1.000 | 200 | 250 | 4,000 | 1,500 | Ba |
| Rb | 1.49 | 5 | 300 | 15 | 50 | 50 | 200 | X | 200 | 10 | 10 | 300 | 200 | Rb |
Be (10), Mo (5), Sn (15), In (1), La (40), Ag (1) and Tl (2) were not detected (approximate limits of sensitivity in brackets).
[The section below cannot be correctly rendered as it contains complex formatting. See the image of the page for a more accurate rendering.]
| 8871 | 8873 | 8932 | 8776 | 8768 | 8791 | 8800 | 8859 | 8829 | 8819 | 8817 | |
|---|---|---|---|---|---|---|---|---|---|---|---|
| Ba/K | .006 | .0015 | .004 | .04 | .02 | .0001 | .007 | .005 | .006 | .02 | .01 |
| Ba/Ca | .005 | .0004 | .002 | .04 | .03 | .00007 | .01 | .004 | .02 | .7 | .1 |
| Sr/K | .04 | .003 | .007 | .07 | .08 | .0008 | .001 | .0004 | .0008 | .0002 | .0002 |
| Sr/Ca | .03 | .0008 | .001 | .08 | .1 | .0005 | .002 | .0003 | .0025 | .006 | .001 |
| Ba/Sr | .2 | .5 | .6 | .5 | .3 | .2 | 7 | 15 | 9 | 100 | 70 |
| Rb/K | .006 | .001 | .002 | .001 | .003 | — | .0025 | .004 | .004 | .003 | .0025 |
Note.—For descriptions of specimens see opposite.

[The section below cannot be correctly rendered as it contains complex formatting. See the image of the page for a more accurate rendering.]
| 8871 | 8873 | 8932 | 8776 | 8768 | 8791 | 8800 | 8859 | 8829 | 8819 | 8817 | 8818 | 9108 | 9051 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| SiO2 | 57.13 | 56.56 | 55.75 | 62.91 | 65.59 | 60.90 | 64.71 | 73.96 | 78.07 | 77.82 | 80.46 | |||
| TiO2 | 1.27 | 1.52 | 1.34 | 0.37 | 0.38 | 0.21 | 0.41 | 0.24 | 0.13 | 0.17 | 0.13 | |||
| Al2O3 | 16.03 | 15.24 | 16.16 | 13.85 | 13.76 | 16.30 | 15.22 | 12.99 | 11.68 | 10.03 | 8.89 | |||
| Fe2O3 | 3.17 | 3.28 | 1.25 | 1.01 | 1.05 | 2.18 | 2.85 | 1.95 | 1.36 | 1.60 | 1.63 | |||
| FeO | 5.35 | 5.46 | 7.34 | 2.28 | 2.43 | 0.55 | 1.00 | 0.49 | 0.30 | 0.63 | 0.46 | |||
| MnO | 0.10 | 0.12 | 0.12 | 0.08 | 0.04 | 0.03 | 0.02 | tr. | tr. | 0.02 | 0.01 | |||
| MgO | 2.51 | 2.60 | 3.87 | 1.42 | 1.18 | 0.28 | 0.82 | 0.40 | 0.04 | 0.40 | 0.39 | |||
| CaO | 4.00 | 3.77 | 3.50 | 3.19 | 3.13 | 5.45 | 3.01 | 1.97 | 0.44 | 0.25 | 0.64 | |||
| Na2O | 3.17 | 5.38 | 4.39 | 1.24 | 1.76 | 0.42 | 2.45 | 5.42 | 4.89 | 0.85 | 1.21 | 1.41 | 5.10 | 6.13 |
| K2O | 2.79 | 0.92 | 1.59 | 2.71 | 3.25 | 2.54 | 4.46 | 1.33 | 1.31 | 6.54 | 4.59 | 10.47 | 1.54 | 1.04 |
| H2O+ | 3.27 | 2.54 | 3.51 | 7.80 | 5.37 | 8.22 | 4.01 | 1.06 | 1.07 | 1.03 | 0.98 | |||
| H2O- | 0.78 | 0.75 | 0.72 | 2.81 | 1.68 | 2.70 | 0.92 | 0.28 | 0.27 | 0.32 | 0.32 | |||
| P2O5 | 0.23 | 0.22 | 0.30 | 0.12 | 0.07 | 0.05 | tr. | tr. | tr. | tr. | 0.02 | |||
| CO2 | 0.09 | 1.37 | 0.44 | nt.fd. | 0.05 | nt.fd. | nt.fd. | nt.fd. | nil | nil | nil | |||
| BaO* | 0.06 | 0.00 | 0.02 | 0.34 | 022 | 0.00 | 0.11 | 0.02 | 0.03 | 0.45 | 0.17 | |||
| Total | 99.95 | 99.73 | 100.30 | 100.13 | 99.96 | 99.83 | 99.99 | 100.11 | 99.59 | 100.11 | 99.90 | |||
| Sp. Gr. | 2.70 | 2.74 | 2.74 | 2.40 | 2.49 | 2.38 | 2.55 | 2.66 | 2.61 | 2.61 | 2.59 |
| 8871. | Andesine-bearing augite-andesite tuff with a little healandite after glass. Bed NR1, North Range, Taringatura Survey District, Southland. |
| 8873. | Albitized, meta-andesite lithic tuff. Bed NR1. |
| 8932. | Albitic tuffaceous greywacke. Bed NR5. |
| 8776. | Fine-grained, heulanditized vitric tuff. Bed NR7. |
| 8768. | Coarse-grained, heulanditized vitric-crystal tuff. Bed NR2. |
| 8791. | Fine-grained laumontitized vitric tuff. Bed NR5. |
| 8800. | Coarse-grained laumontitized vitric-Crystal tuff, with a small amount of secondary quartz and feldspars. Bed NR2. |
| 8859. | Quartz-albite-adularia-pumpellyite metasomatite, albite-rich phase. Bed NR2. |
| 8829. | Ditto. Albite-rich phase. Bed NR2. |
| 8819. | Ditto. Adularia-rich phase. Bed NR2. |
| 8817. | Ditto. Adularia-rich phase. Bed NR2. |
| 8818. | Ditto. Concentration of adularia-rich lapilli. |
| 9108. | Analcime-rich tuffaceous greywacke, Kaihiku Gorge, Southland. |
| 9051. | Analcime-rich impure crystal-vitric tuff (Otamitan), Wether Hill, Taringatura. |
[Footnote] * Spectrographic determinations by Dr. Nockolds.

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| 8871 | 8873 | 8932 | 8776 | 8768 | 8791 | 8800 | 8859 | 8829 | 8819 | 8817 | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Q | 14.0 | 11.8 | 8.0 | 35.0 | 33.2 | 36.7 | 25.6 | 33.0 | 43.5 | 46.3 | 53.7 | |
| C | 1.3 | 2.2 | 2.5 | 3.1 | 1.7 | 3.2 | 0.8 | — | 1.4 | 0.7 | 0.6 | |
| Or | 16.6 | 5.5 | 9.4 | 16.1 | 19.3 | 15.1 | 26.4 | 7.9 | 7.8 | 38.8 | 27.2 | |
| Ce | 0.1 | — | 0.1 | 0.8 | 0.5 | — | 0.2 | 0.1 | 0.1 | 1.0 | 0.4 | |
| Ab | 26.5 | 45.6 | 37.2 | 10.5 | 14.9 | 3.6 | 20.6 | 46.0 | 41.4 | 7.2 | 10.3 | |
| An | 17.9 | 8.6 | 12.7 | 15.1 | 14.8 | 26.7 | 14.9 | 7.1 | 2.2 | 1.2 | 3.2 | |
| Wo | — | — | — | — | — | — | — | 1.0 | .— | — | — | |
| Di | En | — | — | — | — | — | — | — | 1.0 | — | — | — |
| Hy | En | 6.3 | 6.5 | 9.7 | 3.5 | 2.9 | 0.7 | 2.2 | 0.0 | 0.1 | 1.0 | 1.0 |
| Fs | 5.3 | 5.0 | 10.5 | 2.9 | 3.1 | — | — | — | — | — | — | |
| Mt | 4.6 | 4.7 | 1.8 | 1.5 | 1.5 | 1.3 | 2.1 | 0.9 | 0.6 | 2.0 | 1.1 | |
| H | — | — | — | — | — | 1.3 | 1.4 | 1.3 | 0.9 | 0.2 | 08 | |
| Il | 2.4 | 2.9 | 2.5 | 0.7 | 0.7 | 0.4 | 0.8 | 0.5 | 0.2 | 0.3 | 0.2 | |
| Ap | 0.5 | 0.5 | 0.7 | 0.3 | 0.2 | 0.1 | — | — | — | — | 0.1 | |
| Cc | 0.2 | 3.1 | 1.00 | — | 0.1 | — | — | — | — | — | — | |
| 4.1 | 3.3 | 4.2 | 10.6 | 7.0 | 10.9 | 4.9 | 1.3 | 1.3 | 1.4 | 1.3 | ||
| H2O± | 99.8 | 99.7 | 100.3 | 100.1 | 99.9 | 100.0 | 99.9 | 100.1 | 99.5 | 100.1 | 99.9 |
