Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schoolsLuquer, Lea McIlvaine
Science
Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schools
Luquer, Lea McIlvaine
Petrology -- Laboratory manuals
Footnote 158:
Have the convergent lens or condenser lowered and the analyzer out
during this test.
Footnote 159:
The minerals are grouped according to the maximum interference colors
given by sections of the thickness of 0.03 mm.
Footnote 160:
In the case of very small crystals, the centering must be accurate and
a cover with a small hole in the center, should be placed over the top
of the tube. In this way the eye is brought directly over the axis of
the microscope and figures can be observed from very minute crystals.
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TRANSCRIBER’S NOTES
Page Changed from Changed to
80 occurs as an alternation product occurs as an alteration product
of anhydrite. Gypsum is soluble of anhydrite. Gypsum is soluble
in hydrochloric in hydrochloric
136 longer the higher the percentage longer the higher the percentage
of calcium in the solution of sodium in the solution
● Typos fixed; non-standard spelling and dialect retained.
● The author used the old chemical symbol (Fl) for Fluorine.
● Corrected the Errata with the exception of the last paragraph
"Corrections for mean indices of refraction in Scheme (insert
folder)".
● Used numbers for footnotes, placing them all at the end of the last
chapter.
● Enclosed italics font in _underscores_.
● Enclosed bold font in ▄lower half block▄.
● The caret (^) serves as a superscript indicator, applicable to
individual characters (like 2^d) and even entire phrases (like
1^{st}).
● Subscripts are shown using an underscore (_) with curly braces { },
as in H_{2}O.
Public-domain text, read in full here on John Shaqi.
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