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Home > Sciences & Environment > Earth sciences > Geology, geomorphology and the lithosphere > Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield
Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield

Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1908 Excerpt: ...present in the rock. Zircon, apatite, epidote, and chalcedony present as secondary minerals. A little fresh, clear, and bright secondary hornblende is to be seen at the edge of some weathered masses of the same mineral. 8327 Sec. 907. Quartz Diorite near Elverdton Dam. This is a mottled rock of medium grain composed of masses of dark green or blue hornblende and white or greenish plagioclase. Under the microscope the rock is seen to consist of plagioclase, hornblende, and quartz with ilmenite (leucoxene) and apatite. As alteration products or secondary minerals may be mentioned epidote, chalcedony, secondary hornblende and chlorite. Plagioclase is present as the chief constituent, and it is very cloudy, so that it does not give good polarisation reactions, still its outline is very distinct, and suggests this mineral rather than orthoclase. It often contains small inclusions of the ferro-magnesian minerals present in the rock. Hornblende is present in two ages, the one brownish in colour and much iron-stained is idiomorphic and is fairly plentiful. In places it is changing into a bright green and fresh-looking hornblende, the nature of which can easily be determined on examining crystals placed adjacent to quartz and felspar. Quartz is very nearly as plentiful as the original hornblende. It contains numerous inclusions consisting of apatite, etc. Associated with it are many masses of chalcedony. A fair amount of ilmenite, changing into leucoxene, also epidote, chlorite, apatite, and zircon are present. 8359 Sec. 910. Quartz Diorite. 25 chains N.W. of N.W. corner of G.M.L. 101, Ard Patrick. This is a medium-grained granitic rock, the chief constituents being white plagioclase felspar, at times inclined to be greenish in hue, and dark green hornblende which i...


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Product Details
  • ISBN-13: 9781130187588
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 54
  • Spine Width: 3 mm
  • Width: 189 mm
  • ISBN-10: 1130187586
  • Publisher Date: 01 Mar 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 113 gr


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Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield
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Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield
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Report Upon the Auriferous Deposits of Barrambie and Errolls (Cue District) and Gum Creek (Nannine District) in the Murchison Goldfield Volume 34; Also Wiluna (Lawlers District) in the East Murchison Goldfield

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