Proceedings of the Royal Society of Victoria

Cover Proceedings of the Royal Society of Victoria
Proceedings of the Royal Society of Victoria
Royal Society of Victoria (Melbourne, Vic.)
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The felspar appears to be exclusively orthoclase, and there is considerable intergrowth of quartz and felspar. Hornblende is absent.
The basic secretions occur in small ovoid masses rarely more than a few feet in diameter. The normal form is a fine-grained dark rock in which biotite is the prevailing mineral, variation from this type arises from the occurrence in the rock of porphy- ritic masses of pink felspar. Examined microscopically, the rock is seen to be a crystalline granular aggregate o
...f mica, quartz and orthoclase, with a small amount of hornblende. [One slide failed to yield any traces of hornblende]. The almost entire absence of a triclinic felspar is noticeable. Sphene and apatite are both present in small quantities.
Dromana, — Quarry on Arthur's Seat. — A fine-grained syenite in which a pink felspar, quartz and mica are visible. In the thin slide the monoclinic felspar is seen to preponderate over the triclinic, it is frequently twinned according to the Carlsbad law.


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