Micropetrology for Beginners; An Introduction to the Use of the Microscope in the Examination of Thin Sections of Igneous Rocks
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Micropetrology for Beginners; An Introduction to the Use of the Microscope in the Examination of Thin Sections of Igneous Rocks

Micropetrology for Beginners; An Introduction to the Use of the Microscope in the Examination of Thin Sections of Igneous Rocks


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This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1912 edition. Excerpt: ...of hypersthene. like hypersthene, it extinguishes straight. It frequently alters to a fibrous substance known as bastite, resembling it in other microscopical properties. A very typical accessory mineral in lherzolite and other peridotites is picotite. Picotite has a very high refractive index, and hence has a very deep black border and rough surface, but between crossed nicols it remains dark for all positions of the slide--i.e. it is isotropic. It is usually a very dark brown colour, and occurs in granules rather than in crystals, though it is moulded by all the other constituents of the rock. It belongs to the spinel group, and other spinels differ from it principally in colour, mode of occurrence, and chemical composition. Thus pleonaste is green and frequently occurs in polygonal crystals; chromite is darker in colour than picotite, being usually opaque in any but the thinnest slices. In the picrites and peridotites we have the antithesis of the acid rocks; they are therefore termed ultrabasic. Instead of free quartz, we find free bases, such as the iron ores and spinels, whilst the silicates themselves are chiefly varieties of olivine which contain twice as much of the bases as the hornblendes and augites of the intermediate rocks. CHAPTER V THE HYPABYSSAL ROCKS AND THE STUDY OF THE GROUNDMASS AND PHENOCRYSTS The hypabyssal rocks are less coarsely crystalline than the plutonic rocks of the last two chapters, and form a perfect transition from these to the volcanic rocks, which are to be described later. Riebeckite Riebeckite Microgranite.--The riegranite. beckite microgranite of Ailsa Craig, Firth of m"it-e Clyde, Scotland (see Figs. 12 and 13), may be Microperthite, grst examined. Quartz. On examining a slide of this rock by...


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Product Details
  • ISBN-13: 9781234382568
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 24
  • Spine Width: 1 mm
  • Width: 189 mm
  • ISBN-10: 1234382563
  • Publisher Date: 22 Jan 2013
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 64 gr


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Micropetrology for Beginners; An Introduction to the Use of the Microscope in the Examination of Thin Sections of Igneous Rocks
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