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Copyright by Nysha Chaderton 2009 - The University of Texas at ...

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Framework grains<br />

Quartz<br />

Feldspar<br />

Rock Fragments<br />

Accessory Minerals<br />

Porosity*<br />

Authigenic Minerals<br />

Pore F illing<br />

P olycrystalline<br />

Monocrystalline<br />

Factured Quartz grain<br />

Quartz with recycled quartz overgrowths<br />

K Feldspar (stained yellow) tartan twinning<br />

Ca‐ Plagioclase (stained pink/red) polysynthetic twinning<br />

Na‐Plagioclase (doesn't take stain)<br />

Altered Volcanic Rock fragments‐ some pyrite,<br />

feldspars altered to clay<br />

Chert<br />

Argillaceous Rock fragments<br />

Muscovite<br />

Biotite<br />

Zircon<br />

Glauconite<br />

Pyrite<br />

Primary Intergranular<br />

Secondary Intragranular<br />

Secondary Moldic<br />

Secondary Fractured Intragranular<br />

Quartz overgrowths<br />

K aolinite<br />

Chlorite<br />

Hem<strong>at</strong>ite<br />

Breedy's CMRA ITR9 ITR14 SGRF1C SGRF9 SGRF11B SGRF19C WRA WRB<br />

2 4 0 0 2 4 5 0 0 0<br />

7 30 19 22 40 31 30 2 15 4<br />

80 32 45 30 72 74 60 85 90 106<br />

3 4 3 5 4 8 1 8 20 11<br />

6 10 10 16 7 8 7 4 6 4<br />

15 16 24 2 0 11 7 0 2<br />

0<br />

1 3 3 2<br />

1 2 2<br />

1 1 1<br />

5 2 3 5 2 4 8 3 0<br />

0 1 0 1 1 0<br />

0 0 0 0 0 0<br />

194<br />

1 2<br />

36 30 39 27 44 46 35 50 45 50<br />

11 2 8 4 12 0 4 2<br />

1 3 2 1<br />

12 7 10 7 5 5 21 10 15<br />

5 10 5 4 1 0 5 3<br />

1 11 4 5 4 1 7 1<br />

15 27 24 9 16 10 3 9 10 6<br />

K aolinite<br />

6 56 20<br />

Chlorite<br />

5 5<br />

Grain replacement<br />

Total 200 200 200 200 200 200 200 200 200 200<br />

Table A.1: Table shows results <strong>of</strong> point counting <strong>of</strong> the ten samples selected for petrographic examin<strong>at</strong>ion <strong>of</strong> the Scotland Form<strong>at</strong>ion. Oversized Pl<strong>at</strong>e (11x17) requires plotter or printer with tabloid printing.

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