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File:Transactions of the Royal Society of New Zealand (1920) (14742055896).jpg

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Identifier: transactionsofro19200roya (find matches)
Title: Transactions of the Royal Society of New Zealand
Year: 1920 (1920s)
Authors: Royal Society of New Zealand
Subjects: Science
Publisher: Wellington, N.Z. : The Society
Contributing Library: Brigham Young University Hawaii, Joseph F. Smith Library
Digitizing Sponsor: Consortium of Church Libraries and Archives

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Fig. 1.—Graphic intergrowth of quartz and orthoclase in pegmatite. Boulder from conglomerate in oldermass, Mine Bay Creek. Crossed nicols. X 2G.Fig. 2.—Granulite with garnet (black, in centre) from conglomerate in oldermass, Mine Bay Creek. Crossed nicols. X 26.Fig. 3.—Granulite from conglomerate in oldermass, Mine Bay Creek. Crossed nicols. X 26.Fig. 4.—Hypersthene with resorbed borders in second period andeside, Kaitoke Valley. X 26.Fig. 5.—Section of a typical second period andesite, showing a phenocryst oi hypersthene and the characteristic fine groundmass. X 26.Fig. 6.—Phenocrysts of zoned plagioclase and of quartz in quartz-porphyry from headwaters of Mine Bay Creek. Crossed nicols. X 26. Trans. N.Z. Inst., Vol. LIU. Plate XXVII
Text Appearing After Image:
Fig. Fig.Fig. Fig. Fig. 1.—A porphyrite from the dyke complex of Mine Bay. Part of a large plagio-clase crystal is recognizable, and the irregular nature of the coarse ground-mass can just be discerned. Crossed nicols, X 26. 2.—Sagenitic pseudomorph after biotite in porphyrite from Mine Bay area. X 150. 3.—Quartz-mica-porphyrite from intrusion near old copper-mine. Phenocrystsof biotite and plagioclase can be seen. Crossed nicols. X 26. 4.—A quartz phenocryst from a hornblende-biotite-quartz-porphyrite formingintrusion a little south of Miners Head. The crystal shows a distinctcorrosion border. Crossed nicols. X 26. 5.—Pilotaxitic andesite from dyke in oldermass of Mine Bay Creek. Crossednicols. X 26. Bartrum.—Geology of Great Barrier Island. 125 Quartz forms about half the bulk of the minerals, though cryptoperthiteis fairly plentiful along with orthoclase. The only other minerals are alittle plagioclase and some flakes of biotite. It is possible that this rockis the true

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Author Royal Society of New Zealand
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  • bookid:transactionsofro19200roya
  • bookyear:1920
  • bookdecade:1920
  • bookcentury:1900
  • bookauthor:Royal_Society_of_New_Zealand
  • booksubject:Science
  • bookpublisher:Wellington__N_Z____The_Society
  • bookcontributor:Brigham_Young_University_Hawaii__Joseph_F__Smith_Library
  • booksponsor:Consortium_of_Church_Libraries_and_Archives
  • bookleafnumber:199
  • bookcollection:brighamyounguniversityhawaii
  • bookcollection:americana
Flickr posted date
InfoField
28 July 2014


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