Maximum and minimum water contents of granitic melts generated in the crust: A reevaluation and implications

Lithos

Volumn 56, Issue 1, 2001, Pages 1-14

  Holtz, F ^a   Johannes, W ^a   Tamic, N ^a   Behrens, H ^a  

^a LEIBNIZ UNIVERSITY HANNOVER   (Germany)

Author keywords

Granite; Liquidus; Rhyolite; Silicate melt; Viscosity; Water solubility

Indexed keywords

GRANITE; RHYOLITE; SILICATE MELT; WATER;

EID: 0035069397     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0024-4937(00)00056-6     Document Type: Article

References (51)

1. Granitic melt viscosities: Empirical and configurational entropy models for their calculation
2. Liquidus temperatures and phase compositions in the system Qz-Ab-Or at 5 kbar and very low water contents
3. The effect of anhydrous composition on water solubility in granitic melts
4. 8 melts (M=Li, Na, K, Rb)
5. Solubility of carbon dioxide and water in rhyolitic melt at 850°C and 750 bars
6. The importance of volatile constituents
7. Equilibrium properties of granite pegmatite magmas
8. 2O in phonolitic melts
9. Origin of peraluminous granites and granodiorites, Iberian massif, Spain: An experimental test of granite petrogenesis
10. Constraints on melting and magma production in the crust
11. Origin and crystallization of some peraluminous (S-type) granitic magma
12. Origin of an A-type granite: Experimental constraints
13. An experimental study of a lower Proterozoic A-type granite from the Eastern Amazonian craton
14. 2O in melts in the system
15. 2
16. Solubility of water in albite melt determined by the weight-loss method
17. The role of fluids in the formation of High Himalayan leucogranites
18. Viscosities of hydrous leucogranitic melts: A non-Arrhenian model
19. Application of experimental results to C-O-H species in natural melts
20. Maximum and minimum water contents of granitic melts: Implications for chemical and physical properties of ascending magmas
21. 2O on liquidus phase relations in the haplogranitic system at 2 and 5 kbar
22. Water solubility in haplogranitic melts. Compositional, pressure and temperature dependence
23. 2O to 35 kilobars, dry and with excess water
24. 2
25. The granite system at pressure of 4 to 10 kilobars
26. 2O systems
27. Partial melting of metagreywackes. Part II. Compositions of minerals and melts
28. 2O in magmas to 3 kilobars
29. 2O-undersaturated haplogranitic melts
30. 2 in NaA1 silicate melts
31. 2 fluid in silicate liquids
32. Dehydration melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar
33. Effects of P, f(O2) and Mg/Fe ratio on dehydration melting of model metagreywackes
34. Experimental constraints on Himalayan Anatexis
35. 8
36. Experimental crystallization of leucogranitc magmas
37. The viscosity of Himalayan leucogranites: Implications for mechanisms of granitic magma ascent
38. Phase equilibrium constraints on the viscosity of silicic magmas. 1. Volcanicplutonic comparison
39. Preliminary report on equilibrium-relations between feldspathoids, alkali feldspars and silica
40. Viscosities of magmatic liquids: An empirical method of prediction
41. The influence of bulk composition on the speciation of water in silicate glasses
42. Partial fusion of basic granulites at 5 to 15 kbar: Implications for the origin of TTG magmas
43. 2O at 4kbar
44. Melt production during granulite-facies anatexis: Experimental data from 'primitive' metasedimentary protoliths
45. 2O fluid phase
46. 2O-undersaturated granitic liquids
47. 2O
48. Water solubility in melts of alkali feldspar composition at 5 kbar, 950°C
49. The viscosity of hydrous granites: Comparison of real and model compositions
50. Experimental study of the effect of temperature on water solubility in natural rhyolite melt to 100 MPa
51. 2O in rhyolitic glasses and melts: Measurement, speciation, solubility, and diffusion