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Water-saturated melting relations to 5 kilobars of three Leucite Hills lavas

โœ Scribed by M. Barton; D. L. Hamilton


Book ID
104747405
Publisher
Springer
Year
1978
Tongue
English
Weight
821 KB
Volume
66
Category
Article
ISSN
0010-7999

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โœฆ Synopsis


The water-saturated phase relations of three Leucite Hills lavas have been determined at pressures up to 5 kb. Phlogopite is the major primary liquidus phase in orendite and wyomingite at pressures, > 1 kb, but clinopyroxene and olivine are the major primary liquidus phases in madupite at pressures up to 5 kb. Leucite is a liquidus phase in all three magmas at pressures <0.5 kb. The experimental results are in reasonable agreement with the inferred crystallization sequences for the Leucite Hills lavas and have applications to the crystallization and differentiation of potassium-rich magmas within the crust.


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