A Method of Petrographic Analysis Based Upon Chromatic Interference With Thin S

Homer Munro Derr

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0090 Epidote . . .
. 0. 0545 Cordierite . .
. . 0. 0090 Anhydrite . .
. 0. 0430 Axinite . . 0. 0090 Muscovite . .
. 0. 0420 Orthoclase . . 0. 0080 Olivine 0. 0360 Albite . . .
0. 0080 Scapolite . 0. 0360 Beryl . .
0. 0073 Diopside . . .
. 0. 0335 Plagioclase . . 0. 0071 Cancrinite .
. 0. 0289 Zoisite .
0. 0060 Tremolite . . .
. 0. 0265 Melilite . .
. . 0. 0058 Hornblende . .
. 0. 0240 Nephelite . .
. . 0. 0049 Augite ....
. 0. 0220 Elaeolite . .
. . 0. 0047 Sillimanite . .
. 0. 0220 Apatite . ....
. . 0. 0042 Glaucophane . .
. 0. 0216 Vesuvianite .
. . 0. 0020 Brucite . . .
. 0. 0210 Apophyllite .
. . 0. 0019 Tourmaline . .
. 0. 0189 Leucite . .
. . 0. 0010 Chlorite . .
. . 0. 0010 16 Plate 2.
PLATE 2. (Crossed Nicols. ) Chalcedony, Section cut at right angles to the length of a stalactite ; X 100 diameters. Central sections through the concretions give a spherulitic interference cross. Radial fibers appear to be uniaxial, since extinction is complete in fibers parallel to planes of vibration of polarizer and analyzer, i.

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