Sample: 53-B-13
| Sample ID: | 53-B-13 [1] |
| Station ID: | 53-B-13 |
| AT Num: | |
| Volcano: | Makushin |
| Possible source: | |
| Eruption: | |
| Collector: | Barnett, H. F. J. |
| Date sampled: | 1953-01-01 |
| Sample type 1: | Countryrock |
| Color: | |
| Final unit: | |
| Text Description: | Granogabbro occurring one-third mile from the Beaver pluton contact on the east side of Final Bay. The texture is hypidiomorphic and the groundmass is myrmekitic. Felsic minerals compose 80-85 percent of the rock: 7-10 percent quartz, 15-25 percent alkali feldspar partially altered to kaolin (2-3 percent), and 50-58 percent plagioclase partly altered to sericite (about 5 percent) and epidote-clinozoisite (about 1 percent). The plagioclase composition, by extinction angle, is A62 [mean of 28 crystals, standard deviation is 10 percent An, average amount of zoning per individual plagioclase crystal is 2 percent An per crystal], by index oils, is An54. Mafic minerals compose 15-20 percent: 10-13 percent uralitic hornblende (probably 85 percent of this after pyroxene, 15 percent after biotite) partly altered to penninite (0.5-1.5 percent). 0.5-1.5 percent sphene partly altered to leucoxene (0.1 percent), 4-6 percent magnetite, and <1 percent apatite. The discrepancy in plagioclase composition is probably due to sodium in the alkalic feldspar, and potassium in the plagioclase (?). |
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