Composition of aqueous fluid coexisting with mantle minerals at high pressure and its bearing on the differentiation of the Earth's mantle

Geochimica et Cosmochimica Acta

Volumn 66, Issue 12, 2002, Pages 2273-2285

  Mibe, Kenji ^a   Fujii, Toshitsugu ^a   Yasuda, Atsushi ^a  

^a UNIVERSITY OF TOKYO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

AQUEOUS SOLUTION; DIFFERENTIATION; FLUID FLOW; MANTLE CHEMISTRY;

EID: 0036309776     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(02)00856-6     Document Type: Article

References (66)

1. Abundances of the elements: Meteoritic and solar
2. 2O at 2.0-3.0 GPa and 900-1100°C, and application to models of subduction zone processes
3. Compositions of near-solidus peridotite melts from experiments and thermodynamic calculations
4. Quartz-coesite transition revisited: Reversed experimental determination at 500-1200°C and retrieved thermochemical properties
5. Volatiles on Earth and Mars: A comparison
6. 2O to 60 kbar
7. Experimental tests of low degree peridotite partial melt compositions: Implications for the nature of anhydrous near-solidus peridotite melt at 1 GPa
8. Vein-plus-wall-rock melting mechanisms in the lithosphere and the origin of potassic alkaline magmas
9. Composition of fluid coexisting with olivine and pyroxene at high pressure: The role of water on the differentiation of the mantle
10. The role of volatiles in the transition zone
11. Partitioning of elements among two silicate perovskites, superphase B, and volatile-bearing melt at 23 GPa and 1500-1600°C
12. Petrogenesis of mid-ocean ridge basalts
13. Garnet and pyroxene in the mantle: A test of the majorite fractionation hypothesis
14. 2O in silicate melts
15. 2O up to 15 GPa
16. 2O and melting in subduction zones
17. The abundances of major, minor and trace elements in the earth's mantle as derived from primitive ultramafic nodules
18. 3 (I): Eutectic relations up to 7 GPa
19. Experimental determination of element partitioning between silicate perovskites, garnets and liquids: Constraints on early differentiation of the mantle
20. 3 perovskite and liquid determined by direct measurements
21. 2O-saturated mantle peridotites to 11 gigapascals
22. Genesis of high Mg# andesites and the continental crust
23. 2O
24. Origin of materials in the Earth's interior and their layered distribution
25. Effect of water on the melting of enstatite
26. Cumulate maturation and melt migration in a temperature gradient
27. 2O system at 3 to 12 GPa
28. Is phase A relevant to the Earth's mantle?
29. 2O in the lower crust and upper mantle
30. Element partitioning between Mg-perovskite, magnesiowüstite, and silicate melt at conditions of the Earth's mantle
31. Compositions of aqueous fluid coexisting with mantle minerals at high pressures: The role of water on the differentiation of the mantle
32. Connectivity of aqueous fluid in the Earth's upper mantle
33. Control of the location of the volcanic front by aqueous fluid connectivity in the mantle wedge
34. Melting of a hydrous mantle: I. Phase relations of natural peridotite at high pressures and temperatures with controlled activities of water, hydrogen, and carbon dioxide
35. Alkali aluminosilicate-saturated aqueous fluids in the earth's upper mantle
36. 2 at 15 kbar
37. 2O at 15 kbar
38. The primordial terrestrial magma ocean and its implications for stratifications of the mantle
39. 4 up to 15 GPa
40. Composition of the core. I. Solubility of oxygen in molten iron at high temperatures
41. Melting of a model chondritic mantle to 20 GPa
42. Reversals of the orthoenstatite-clinoenstatite transition at high pressures and high temperatures
43. Ca/Al ratio and composition of the Earth's upper mantle
44. The chemical composition and origin of the Earth
45. Composition of the core and implications for origin of the earth
46. Making the continental crust
47. Compositions of aqueous fluid in equilibrium with pyroxenes and olivines at mantle pressures and temperatures
48. Fluids in equilibrium with peridotite minerals: Implications for mantle metasomatism
49. Phase relations of a serpentine composition between 5 and 14 GPa: Significance of clinohumite and phase E as water carriers into the transition zone
50. 2O under upper mantle conditions
51. Melting of a dry peridotite KLB-1 up to 14 GPa: Implications on the origin of peridotic upper mantle
52. Compositional dependence of dihedral angles in partially molten systems: Thermostatistical models
53. Migration of fluid phases and genesis of basalt magmas in subduction zones
54. The origin and growth of continents
55. Adcumulus dunite growth in a laboratory thermal gradient
56. Composition of chondrites
57. 2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation
58. The chemical composition of some stony meteorites
59. 4 using synchrotron radiation
60. 2O at high pressures and temperatures-stability field for hydroxyl-chondrodite and 10Å-phase
61. Melting relation of an anhydrous abyssal basalt at high pressure
62. Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa
63. In situ X-ray observations of the coesite-stishovite phase transformation: Reversed phase boundary and kinetics
64. Enstatite-forsterite-water equilibria at elevated temperatures and pressures