Experimental modeling of the cooling history of Apollo 12 olivine basalts.
Colin H. Donaldson, Thomas M. Usselman, Richard J. Williams, G. E. Lofgren
Abstract
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Colin H. Donaldson, Thomas M. Usselman, Richard J. Williams, G. E. Lofgren
Abstract
Open-access reader
An analog of the Apollo 12 olivine vitrophyres has been crystallized in a 1-atm gas-mixing furnace at cooling rates ranging between 1250 and 0.7°/hr and isothermally at degrees of supercooling ranging from 10°C to 325°C. Mineral chemistry, crystal shapes, grain sizes and textures are systematically related to cooling rate and degree of supercooling.
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An analog of the Apollo 12 olivine vitrophyres has been crystallized in a 1-atm gas-mixing furnace at cooling rates ranging between 1250 and 0.7°/hr and isothermally at degrees of supercooling ranging from 10°C to 325°C. Mineral chemistry, crystal shapes, grain sizes and textures are systematically related to cooling rate and degree of supercooling.
Key concepts: Olivine, Ilmenite, Basalt, Geology, Plagioclase, Supercooling, Pyroxene, Mineralogy