The Isomorphism And Thermal Properties of the Feldspars

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J. P. Iddings of the University of Chicago, whose large petrographic experience with mineral crystallites makes his judgment of very exceptional value. His analyses (see Part II) of the slides form an important part of this discussion. We are also indebted to Mr. W. L/indgren of the United States Geological Survey for valuable assistance in the microscopical study of our products.
ANALYSES OF ARTIFICIAL FELDSPARS.
An. AbiAn s .
A Dl An 2 .
AbaAn^ Found.
Calcu- lated.
Found.
Calcu- lated.
Found.
...
Calcu- lated.
Found Calcu- lated.
SiO, 43-33 36. 21 . 29 20. 06 . Ii 43. 28 36. 63 20. 09 47. 10 34- 2 3 15 17. 00 1. 74 47. 18 34-oo 16. 93 1. 87 51. 06 3I-50 . 22 I3-65 3-68 51-30 31. 21 'ia'es 3-79 60. 01 24-95 . 29 7. 09 7-79 59. 81 25-47 6^98 7-73 AloO, Fe. , O, CaO Na 3 O 100. 00 100. 22 IOO. II 100. 13 The constituents used in our syntheses were precipitated calcium carbonate, anhydrous sodium carbonate, powdered quartz (selected crystals), and alumina prepared by the decomposition of ammonium alum.


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