Modern Lithology Illustrated and Defined, for the Use of University, Technical and Civil-Service Students
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Modern Lithology Illustrated and Defined, for the Use of University, Technical and Civil-Service Students

Modern Lithology Illustrated and Defined, for the Use of University, Technical and Civil-Service Students


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Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free. This is an OCR edition with typos. Excerpt from book: PLATE X. Fig. 1. Left-hand semicircle. Dunite, Mount Dun, New Zealand, x 15.?The entire field is here shown to consist of compacted crystals of fresh colourless olivine exhibiting " shagreened " surfaces and fissures of black lines, which, with a higher power, show separated grains of magnetite. Another spinellid also occurs in the form of grains of coffee-brown picotite; while red garnet (p'yrope), not shown in the figure, has also been frequently detected in the rock. Right-hand semicircle. Lherzolite, Etang de Lherz, Pyrenees, x 15. ? This well-known rock may be described briefly as an enstatite-augite-peridotite. The dominant constituent olivine is shown at the equatorial boundary in colourless "shagreened" grains with irregular black fissures, occasioned by the highly re- fringent nature of the mineral coupled with separations of granules of magnetite. At the top apex there is more olivine, which stretches downward along the polar diameter to tail off at the equator. This patch of olivine is seen to be freely traversed by sinuous paths of green serpentine. At the upper right-hand boundary is an intersected patch of deep-brown chromite, limited below by a veinlet of green serpentine, which also penetrates the subjacent crystal of faint-brown enstatite. Lower down, immediately under the olivine already noted, there is another crystal of light-brown rhombic pyroxene (enstatite) characterised by the possession of D a fairly perfect pinacoidal cleavage. The light-green central and inferior crystals are monoclinic pyroxenes (augite) of the nature of chrome-bearing diopside. The lower crystal shows cleavages parallel to the prism, of 87. Fig. 2. divine-Serpentine, Saxony, x 20.?The left-hand half under ordinary, and the right-hand semicircle under parallel, polarised lig...


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Product Details
  • ISBN-13: 9781151746078
  • Publisher: General Books
  • Publisher Imprint: General Books
  • Height: 229 mm
  • No of Pages: 82
  • Spine Width: 5 mm
  • Width: 152 mm
  • ISBN-10: 115174607X
  • Publisher Date: 01 Jan 2010
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 132 gr


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Modern Lithology Illustrated and Defined, for the Use of University, Technical and Civil-Service Students
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