Abstract
A method for conducting successful low pressure (0.3-0.5 GPa) and high temperature (900-1200 °C) experiments in the 19 mm piston-cylinder is presented. The technique is capable of running high fluid/melt experiments with minimum hydrogen loss, attaining precise, reproducible pressures (±10%), and has fast initial quench rates (>150 °C/s). These abilities are invaluable when conducting low pressure, fluid-saturated experiments such as phase equilibria, volatile solubility, and dynamic degassing experiments that are relevant to sub-volcanic magma chamber processes. A double capsule construction is also described that uses a solid oxygen buffer, and minimizes both contamination of the sample by carbon and the loss of iron in the melt to the capsule walls.
© 2015 by Walter de Gruyter Berlin/Boston
Artikel in diesem Heft
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Artikel in diesem Heft
- Footemineite, the Mn-analog of atencioite, from the Foote mine, Kings Mountain, Cleveland County, North Carolina, U.S.A., and its relationship with other roscherite-group minerals
- Element mobility and scale of mass transport in the formation of quartz veins during regional metamorphism of the Waits River Formation, east-central Vermont
- Chemical and physical transfers in an ultramafic rock weathering profile: Part 1. Supergene dissolution of Pt-bearing chromite
- Chemical and physical transfers in an ultramafic rock weathering profile: Part 2. Dissolution vs. accumulation of platinum group minerals
- Comparative Raman spectroscopic study on ilmenite-type MgSiO3 (akimotoite), MgGeO3, and MgTiO3 (geikielite) at high temperatures and high pressures
- A low-pressure–high-temperature technique for the piston-cylinder
- Pressure-induced structural deformation and elastic behavior of wairakite
- Metamorphic vanadian-chromian silicate mineralization in carbon-rich amphibole schists from the Malé Karpaty Mountains, Western Carpathians, Slovakia
- High-temperature deformation of volcanic materials in the presence of water
- Menezesite, the first natural heteropolyniobate, from Cajati, São Paulo, Brazil: Description and crystal structure
- Single-crystal X-ray and Raman investigation on melanophlogite from Varano Marchesi (Parma, Italy)
- Direnzoite, [NaK6MgCa2(Al13Si47O120)·36H2O], a new zeolite from Massif Central (France): Description and crystal structure
- On twinning and microstructures in calcite and dolomite
- Density functional calculations of the electronic structure and optical properties of aluminosilicate polymorphs (Al2SiO5)
- Crystal-size distribution and composition of garnets in eclogites from the Dabie orogen, central China
- Cation order/disorder behavior and crystal chemistry of pyrope-grossular garnets: An 17O 3QMAS and 27Al MAS NMR spectroscopic study
- Analytical transmission electron microscopy study of a natural MORB sample assemblage transformed at high pressure and high temperature
- Barioperovskite, BaTiO3, a new mineral from the Benitoite Mine, California
- The nature of unusual luminescence in natural calcite CaCO3
- Carbonate in igneous and metamorphic fluorapatite: Two type A and two type B substitutions
- The crystal structure of diopside at pressure to 10 GPa
- Electron backscatter diffraction analysis of zircon: A systematic assessment of match unit characteristics and pattern indexing optimization
- Compressibility trends of the clinopyroxenes, and in-situ high-pressure single-crystal X-ray diffraction study of jadeite
- Synthesis and characterization of low-OH– fluor-chlorapatite: A single-crystal XRD and NMR spectroscopic study
- Pressure dependence of the hydrogen-bond geometry in topaz-OD from neutron powder diffraction
- Environments around Al, Si, and Ca in aluminate and aluminosilicate melts by X-ray absorption spectroscopy at high temperature
- The origin of S4+ detected in silicate glasses by XANES
- Effects of ionizing radiation on the hollandite structure-type: Ba0.85Cs0.26Al1.35Fe0.77Ti5.90O16
- Letter. Toward a thermal model for the Skaergaard liquidus