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| Description |
English: "Ghost myrmekite" also occurs in this photomicrograph of Rubidoux Mountain leucogranite. At the extinction position for microcline (black), clusters of quartz blebs (white) occur in faint traces of remnant plagioclase or as isolated oval islands in the microcline. The maximum sizes of the quartz blebs in the microcline match the maximum diameters of quartz vermicules in myrmekite (left side) where plagioclase is white and quartz vermicules are gray. Courtesy Dr. Lorence G. Collins. |
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| Date | |||
| Source | Own work | ||
| Author | Rudolf Pohl | ||
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I, the copyright holder of this work, hereby publish it under the following licenses:    This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 00:58, 13 February 2010 | | 340 × 287 (76 KB) | Techman224 | Removed Border |
| 13:14, 10 September 2009 |  | 640 × 480 (76 KB) | Rudolf Pohl | {{Information |Description={{en|1="Ghost myrmekite" also occurs in this photomicrograph of Rubidoux Mountain leucogranite. At the extinction position for microcline (black), clusters of quartz blebs (white) occur in faint traces of remnant plagioclase or |
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