Содержание
Слайд 2Asst. Prof. Dr. Ayşe pekrioğlu Balkıs
Texture of Rocks
SMALL CRYSTALS --------- COOLED QUICKLY
(because
Asst. Prof. Dr. Ayşe pekrioğlu Balkıs
Texture of Rocks
SMALL CRYSTALS --------- COOLED QUICKLY
(because
![Asst. Prof. Dr. Ayşe pekrioğlu Balkıs Texture of Rocks SMALL CRYSTALS ---------](/_ipx/f_webp&q_80&fit_contain&s_1440x1080/imagesDir/jpg/374063/slide-1.jpg)
of the reduced time for atoms to attain minimum energy configuration)
BIG CRYSTALS ------------- COOLED SLOWLY
Cooling may be so rapid, as in a volcanic eruption, that no crystalline structure develops before solidification:
and an amorphous material such as obsidian (volcanic glass) is formed.
BIG CRYSTALS ------------- COOLED SLOWLY
Cooling may be so rapid, as in a volcanic eruption, that no crystalline structure develops before solidification:
and an amorphous material such as obsidian (volcanic glass) is formed.
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Cyclographic and stereographic projection