The formation of mantle phlogopite in subduction zone hybridization

Contributions to Mineralogy and Petrology

Volumn 79, Issue 4, 1982, Pages 375-380

  Wyllie, Peter J ^a   Sekine, Toshimori ^a  

^a UNIVERSITY OF CHICAGO   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0019924996     PISSN: 00107999     EISSN: 14320967     Source Type: Journal    
DOI: 10.1007/BF01132067     Document Type: Article

References (32)

1. Thermal model for subduction with dehydration in the downgoing slab
2. Dehydration, asthenospheric convection and seismicity in subduction zones
3. Stable isotope, chemical and petrological studies of high-pressure amphiboles and micas: evidence for metasomatism in the mantle source regions of alkali basalts and kimberlites
4. Melting of granite with excess water to 30 kilobars pressure
5. A neodymium and strontium isotopic study of the Mesozoic calc-alkaline granitic batholiths of the Sierra Nevada and Peninsular Ranges, California
6. Subduction and the structure of andesite volcanic belts
7. Crystallization of calc-alkaline andesite under controlled high-pressure hydrous conditions
8. Island arc and continent building magmatism — a review of petrogenic models based on experimental petrology and geochemistry
9. Genesis of calc-alkaline igneous rock suite
10. Crustal evolution by arc magmatism
11. The nature of batholiths
12. Gradients in silicic magma chambers: implications for lithospheric magmatism
13. Volcanic arc magmas: implications of a melting-mixing model for element recycling in the crust-upper mantle system
14. Effect of water on composition of magmas formed at high pressures
15. On the cooling of ascending andesitic magma
16. On the heat and mass transfer from an ascending magma
17. The stability of phlogopite and enstatite at high pressures: a model for micas in the interior of the earth
18. Phase relationships of phlogopite in the system K2O-MgO-CaO-Al2O3-SiO2-H2O to 35 kilobars: a better model for micas in the interior of the earth
19. Trace element partitioning between garnet peridotite minerals and water-rich vapor: experimental data from 5 to 30 kbar
20. Melting of hydrous mantle. I. Phase relations of natural peridotite at high pressures and temperatures with controlled activities of water, carbon dioxide and hydrogen, and II. geochemistry of crystals and liquids formed by anatexis of mantle peridotite at high pressures and temperatures as a function of controlled activities of water, hydrogen and carbon dioxide
21. Composition of the gas phase in Mg2SiO4-SiO2-H2O at 15 kbar
22. Effect of water on olivine stability in tholeiites and production of silica-saturated magmas in the island arc environment
23. Experimental evidence at high pressure for potassic metasomatism in the mantle of the earth
24. Numerical studies of back-arc convection and the formation of marginal basins
25. The origins of potassic magmas: 2. stability of phlogopite in natural spinel lherzolite and in the system KAlSiO4-MgO-SiO2-H2O;CO2 at high pressures and high temperatures
26. Magmas and volatile components
27. Plate tectonics and magma genesis