The water-undersaturated and dry Qz-Ab-Or system revisited. Experimental results at very low water activities and geological implications

Contributions to Mineralogy and Petrology

Volumn 141, Issue 3, 2001, Pages 347-357

  Holtz, F ^a   Becker, A ^a   Freise, M ^a   Johannes, W ^a  

^a LEIBNIZ UNIVERSITY HANNOVER   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ALBITE; GRANITE; ORTHOCLASE; PETROLOGY; PHASE EQUILIBRIUM; QUARTZ; SILICATE MELT;

EID: 0034963525     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s004100100245     Document Type: Article

References (48)

1. Liquidus temperatures and phase compositions in the system Qz-Ab-Or at 5 kbar and very low water activities
2. The effect of anhydrous composition on water solubility in granitic melts
3. 8 (M = Li,Na,K): An interlaboratory study
4. Experimental studies of carbon dioxide in silicate melts: Solubility, speciation, and stable carbon isotope behavior
5. Solubility of carbon dioxide and water in rhyolitic melt at 850°C and 750 bars
6. A two-parameter Margules method for modelling the thermodynamic mixing properties of albite-water melts
7. The importance of volatile constituents
8. Equilibrium properties of granite pegmatite magmas
9. Constraints on melting and magma production in the crust
10. Origin and crystallization of some peraluminous (S-type) granitic magma
11. 2
12. The solubility of carbon dioxide in rhyolitic melts: A quantitative FTIR study
13. An internally-consistent thermodynamic data set for phases of petrological interest
14. 2O on liquidus phase relations in the haplogranite system at 2 and 5 kbar
15. Water solubility in haplogranitic melts. Compositional, pressure and temperature dependence
16. Maximum and minimum water contents of granitic melts generated in the crust: A reevaluation and implications
17. 2O to 35 kilobars, dry and with excess water
18. The influence of the fluid phase composition on the solidus temperatures in the haplogranite system
19. 2O fluids for use in hydrothermal experimentation II. Melting of albite in multispecies fluid
20. 2O
21. The dissolution mechanisms of water in silicate melts; a synthesis of recent data
22. 2O. and P-total in granitic magmas
23. Granitic rocks
24. The granite system at pressure of 4 to 10 kilobars
25. Water solubility and speciation models
26. 2O systems
27. Partial melting of metagreywackes, Part II. Compositions of minerals and melts
28. 2O-undersaturated haplogranitic melts
29. Experimental constraints on the compositional evolution of crustal magmas
30. The speciation of water in haplogranitic glasses determined by in situ near-infrared spectroscopy
31. Phase equilibria and melt productivity in the pelitic system: Implications for the origin of peraluminous granitoids and aluminous granulites
32. 2O loss from hydrous melts during fluid-absent piston-cylinder experiments
33. Dehydration melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar
34. 2O on liquidus phase relations in the haplogranite system at 1 kbar
35. 2O solubility in quartz-feldspar melts
36. Phase equilibrium constraints on the viscosity of silicic magmas. I. Volcanic-plutonic comparison
37. 2O
38. Preliminary report on equilibrium-relations between feldspathoids, alkali feldspars and silica
39. 2O speciation in a diamond-anvil cell
40. The influence of bulk composition on the speciation of water in silicate glasses
41. Partial fusion of basic granulites at 5 to 15 kbar: Implications for the origin of TTG magmas
42. 2O at 4 kbar
43. The speciation of water in silicate melts
44. 2O fluid phase
45. 2O loss during piston-cylinder experiments
46. 2O
47. Experimental study of the effect of temperature on water solubility in natural rhyolite melt to 100 MPa