| 11. | Riebeckite-granites have close affinities to aplites, shown especially in the prevalence of alkali feldspars.
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| 12. | There are also pink and red aplite veins in the igneous complexes up to 5 cm wide.
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| 13. | The aplite is the lowest melting remanent of the granite magma, that is poor in volatiles.
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| 14. | These mountain ranges are represented the three types of rocks : dikes including lamprophyres, pegmatites and aplites.
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| 15. | Intrusions vary widely, from mountain-range-sized batholiths to thin fracture fillings of aplite or pegmatite.
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| 16. | The Pi�gut-Pluviers-Granodiorite is crosscut by many grey, in some places pink microgranitic aplite dikes.
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| 17. | The aplites associated with diorites and quartz-diabases differ in minor respects from the common aplites which accompany granites.
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| 18. | The aplites associated with diorites and quartz-diabases differ in minor respects from the common aplites which accompany granites.
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| 19. | By increase of quartz, aplites pass gradually, in a few localities, through highly quartzose modifications into quartz veins.
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| 20. | The reddish colours of the aplites and the red facies rocks is due to hematite invading the plagioclase and staining it.
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