Rocks And Rock Minerals; a Manual of the Elements of Petrology Without the Use of the Microscope, for the Geologist, Engineer, Miner, Architect, Etc., And for Instruction in Colleges And Schools
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In our eReader you can find the full English version of the book. Read Rocks And Rock Minerals; a Manual of the Elements of Petrology Without the Use of the Microscope, for the Geologist, Engineer, Miner, Architect, Etc., And for Instruction in Colleges And Schools Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Rocks And Rock Minerals; a Manual of the Elements of Petrology Without the Use of the Microscope, for the Geologist, Engineer, Miner, Architect, Etc., And for Instruction in Colleges And Schools
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2. Pyroxene, (M g Fe)Ca(Si0 3 ) 2 . process begins with metallic 3 Plagioclase S mCaAl 2 Si 2 8 - oxides whi ch contain no ' lnNaAlSi 3 8 . silica, that next come the 4. Orthoclase, KAlSi 3 8 . ferromagnesian minerals, yua z, i 2 . ortho and metasilicates, then feldspars which contain more silica and finally quartz or free silica. Thus there tends to crystallize out successively minerals richer and richer in silica. It is not to be understood however that one mineral necessarily finishes its pe...riod of crystallization before another one begins as in A, but rather that they overlap Mag. Pyrox. Plag. Orthoclase. Quartz.
B Mag. Pyrox.
"Bag.
Orthoclase.
Quartz.
as in B, that is, that one may begin before another has finished, and continue after the former has ceased. Expe- rience shows that with orthoclase and quartz the overlap is so great that they crystallize nearly simultaneously, only orthoclase usually begins and quartz finishes.
Insolubility vs. Infusibility. A molten silicate magma is to be regarded as a complex solution of some compounds in others, like a solution of mixed salts in some solvent such- GENERAL PETROLOGY OF IGNEOUS ROCKS 149 as water.
What to read after Rocks And Rock Minerals; a Manual of the Elements of Petrology Without the Use of the Microscope, for the Geologist, Engineer, Miner, Architect, Etc., And for Instruction in Colleges And Schools?
You can find similar books in the "Read Also" column, or choose other free books by Pirsson, Louis V. (Louis Valentine), 1860-1919 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
2. Pyroxene, (M g Fe)Ca(Si0 3 ) 2 . process begins with metallic 3 Plagioclase S mCaAl 2 Si 2 8 - oxides whi ch contain no ' lnNaAlSi 3 8 . silica, that next come the 4. Orthoclase, KAlSi 3 8 . ferromagnesian minerals, yua z, i 2 . ortho and metasilicates, then feldspars which contain more silica and finally quartz or free silica. Thus there tends to crystallize out successively minerals richer and richer in silica. It is not to be understood however that one mineral necessarily finishes its pe...riod of crystallization before another one begins as in A, but rather that they overlap Mag. Pyrox. Plag. Orthoclase. Quartz.
B Mag. Pyrox.
"Bag.
Orthoclase.
Quartz.
as in B, that is, that one may begin before another has finished, and continue after the former has ceased. Expe- rience shows that with orthoclase and quartz the overlap is so great that they crystallize nearly simultaneously, only orthoclase usually begins and quartz finishes.
Insolubility vs. Infusibility. A molten silicate magma is to be regarded as a complex solution of some compounds in others, like a solution of mixed salts in some solvent such- GENERAL PETROLOGY OF IGNEOUS ROCKS 149 as water.
What to read after Rocks And Rock Minerals; a Manual of the Elements of Petrology Without the Use of the Microscope, for the Geologist, Engineer, Miner, Architect, Etc., And for Instruction in Colleges And Schools?
You can find similar books in the "Read Also" column, or choose other free books by Pirsson, Louis V. (Louis Valentine), 1860-1919 to read onlineMoreLess
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