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A Criterion for Predicting Liquid Immiscibility in Silicate Melts
MOST petrologists hold that liquid immiscibility is not a significant process in the genesis of common igneous rocks. Recently, however, petrographie...
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AIIBVI Compounds
Almost all compounds of the AIIBVI type crystallize in such a manner that each atom of one element is located at the center of a regular tetrahedron,... -
Antiferromagnetism in the Vanadium, Manganese and Iron Phosphate Glass Systems
Variable temperature magnetic susceptibility measurements have been made on a series of concentrated vanadium, manganese and iron phosphate glasses.... -
The Properties of Real Gases
The following symbols are used for the principal thermodynamic functions: E (energy), H (heat content), S (entropy), A (Helmholtz free-energy), G... -
Phase Relations in the System Cr-Fe-S
The systems Cr-S and Cr-Fe-S are being systematically investigated by silica tube experiments in which vapor is an inherent phase, as well as by... -
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Nonequilibrium conditions at thermal emission
The process of water evaporation from a clean and a monolayer-coated surface is compared to the similar case of thermionic emission from clean and...
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Immiscibility between Feldspathic and Gabbroic Magmas
Although laboratory experiments in the past have not encouraged hopes of finding terrestrial rocks showing textures resulting from liquid...
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Silicate Immiscibility in the Ancient “Basalts” of the Barberton Mountain Land, Transvaal
The presence of spherical bodies in basaltic rocks strongly suggests that they are globules produced by liquid immiscibility of silicate fractions....
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Origin, age, and composition of meteorites
This paper attempts to bring together and evaluate all significant evidence on the origin of meteorites.
The iron meteorites seem to have formed at...
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Effects of Propellant Injection on Resonant Combustion
A research program has been conducted with the objective of investigating the effect of injector-induced mass flux and mixture ratio-distribution...