Fluid compositions in equilibrium with silica-undersaturated magmas in the system Na2O–Al2O3–SiO2–H2O: clues to the composition of fenitizing fluids
✍ Scribed by Robin F. Preston; Gary Stevens; Terence S. McCarthy
- Publisher
- Springer
- Year
- 2003
- Tongue
- English
- Weight
- 510 KB
- Volume
- 144
- Category
- Article
- ISSN
- 0010-7999
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
The solidus temperatures in the haplogranite-systern NaA1Si3Os-KA1Si3Os-SiO2-H 2 0 -C O 2 have been determined up to 15 kbar for a constant molar ratio of sodium to potassium of 1 : 1 and for fluid compositions ranging from pure water to pure carbon dioxide. The data for the water-saturated solidus
The bioactivity, i.e., bone-bonding ability, of 26 glasses in the system Na 2 O-K 2 O-MgO-CaO-B 2 O 3 -P 2 O 5 -SiO 2 was studied in vivo. This investigation of bioactivity was performed to establish the compositional dependence of bioactivity, and enabled a model to be developed that describes the