Buoyancy-driven propagation of an isolated fluid-filled crack in rock: implication for fluid transport in metamorphism Yoshito Nakashima OriginalPaper Pages: 289 - 295
Thermodynamic data from redox reactions at high temperatures. I. An experimental and theoretical assessment of the electrochemical method using stabilized zirconia electrolytes, with revised values for the Fe-“FeO”, Co-CoO, Ni-NiO and Cu-Cu2O oxygen buffers, and new data for the W-WO2 buffer Hugh St. C. O'NeillMark I. Pownceby OriginalPaper Pages: 296 - 314
Thermodynamic data from redox reactions at high temperatures. II. The MnO-0Mn3O4 oxygen buffer, and implications for the thermodynamic properties of MnO and Mn3O4 Hugh St. C. O'NeillMark I. Pownceby OriginalPaper Pages: 315 - 320
Rutile solubility and mobility in supercritical aqueous fluids John C. AyersE. Bruce Watson OriginalPaper Pages: 321 - 330
Redox states of lithospheric and asthenospheric upper mantle C. Ballhaus OriginalPaper Pages: 331 - 348
Uplift-related retrogression history of aragonite marbles in Western Crete (Greece) Thomas TheyeEberhard Seidel OriginalPaper Pages: 349 - 356
Fluid absent melting of a layered crustal protolith: implications for the generation of anatectic granites Kjell P. SkjerlieAlberto E. Patiño DouceA. Dana Johnston OriginalPaper Pages: 365 - 378
Retrograde deformation within the Carthage-Colton Zone as recorded by fluid inclusions and feldspar compositions: tectonic implications for the southern Grenville Province William M. Lamb OriginalPaper Pages: 379 - 394
Granulite xenoliths from western Saudi Arabia: the lower crust of the late Precambrian Arbian-Nubian Shield Anne V. McGuireRobert J. Stern OriginalPaper Pages: 395 - 408
Evidence for a copper-bearing fluid in magma erupted at the Valley of ten thousand smokes, Alaska Jacob B. Lowenstern OriginalPaper Pages: 409 - 421
Corrections to expressions for calculating mineral components in “Origin of calc-alkaline series lavas at medicine lake volcano by fractionation, assimilation and mixing” and “Experimental petrology of normal MORB near the kane fracture zone: 22°-25°N, mid-atlantic ridge” Timothy L. Grove OriginalPaper Pages: 422 - 424
