๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Water-saturated and undersaturated melting relations of a granite to 35 kilobars

โœ Scribed by C.R. Stern; P.J. Wyllie

Book ID
115853346
Publisher
Elsevier Science
Year
1973
Tongue
English
Weight
447 KB
Volume
18
Category
Article
ISSN
0012-821X

No coin nor oath required. For personal study only.

๐Ÿ“œ SIMILAR VOLUMES

Water-saturated melting relations to 5 k
Water-saturated melting relations to 5 kilobars of three Leucite Hills lavas
โœ M. Barton; D. L. Hamilton ๐Ÿ“‚ Article ๐Ÿ“… 1978 ๐Ÿ› Springer ๐ŸŒ English โš– 821 KB

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

Water-saturated and undersaturated melti
Water-saturated and undersaturated melting relations in a Paricutin andesite and an estimate of water content in the natural magma
โœ David H. Eggler ๐Ÿ“‚ Article ๐Ÿ“… 1972 ๐Ÿ› Springer ๐ŸŒ English โš– 681 KB

Phase relations have been determined for a Paricutin Volcano andesite at pressures to 10 kilobars and for I-I20 contents in the melt of 2 to 10 weight percent. Runs were made under H20-saturated and undersaturated conditions. In undersaturated runs a H20-CO ~ fluid phase was always present. Fugacity