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File:Transactions of the Royal Society of New Zealand (1920) (14578600057).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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ement rocksnow uncovered for examination. In a paper read before the Melbourne meeting of the AustralasianAssociation for the Advancement of Science in January, 1921, the presentwriter adduced arguments in favour of the correlation of the rocks of thepre-Mesozoic land-mass of the North Island with those of the Aoreresystem, so well developed in the South Island. General and Petrographic Description of Onerahi Conglomerate. In December, 1919, in company with Mr. H. T. Ferrar, of the NewZealand Geological Survey, the writer discovered a conglomerate intercalatedin greensands exposed between tide-marks a short distance east of thewharf at Onerahi, near Whangarei. The series of beds of which it is part isprobably Tertiary in age, and is considerably disturbed by folding. Thebeds below the conglomerate are not visible, but above it come about 20 ft.of greensands, and then a gradual passage to an argillaceous limestone * See this volume, pp. 119-20. Trans. N.Z. jt., Vol. LIIT. Plate XXVIII.
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!«. 1.—Granulated (?) quartziie.from conglomerate at Onerahi. Crossed nicols. X 25. 2.—Perthitic feldspar from gneissic granite from conglomerate at Onerahi. Crossed nicol 3.—Plagioclase phenocrysts in granophyre from conglomerate at Onerahi. Crossed nicols.^G. 4.—Granophyric matrix of rock illustrate I by fig. 3 above. Crossed nicols x L33.JIG. 5.—Spherulitic structures in matrix of acidic (?) tuff from Onerahi conglomerate. Crossed nicols. X 133.^ig. G.—Quartz phenocryst from acidic (?) tuff from conglomerate at Onerahi. It contains roundedfragments of finely granophyric hornblende-feldspar rock. Crossed nicols. x 13:5. Face p. 128-1 Bartrum.—A Conglomerate at Onerahi. 129 similar to the very extensive limestone of the North Auckland area usuallyspoken of as the hydraulic limestone. The question of its age is stillunsettled. The band of conglomerate is lensoid, ranging up to about 5 ft. in depth,and is exposed standing steeply on edge for about 15 yards. Its pebblesan

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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:204
  • bookcollection:brighamyounguniversityhawaii
  • bookcollection:americana
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28 July 2014
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