Zobrazeno 1 - 10
of 156
pro vyhledávání: '"Piston-cylinder apparatus"'
Autor:
Silvio Roberto Farias Vlach, Andrés Fabián Salazar-Naranjo, Johan Santiago Torres-Corredor, Paulo Rafael de Carvalho, Guilherme Mallmann
Publikováno v:
Brazilian Journal of Geology, Vol 49, Iss 1 (2019)
Abstract We present pressure calibration results for piston-cylinder –” and 1” high temperature furnace assemblies in the 200-600 MPa range aiming to expand its applicability to simulate upper crustal conditions. The furnace assemblies were mad
Externí odkaz:
https://doaj.org/article/936eb103f5ea4db0be7bc6617db9d2d9
Publikováno v:
Geochimica et Cosmochimica Acta. 310:47-60
Element diffusion in silicate melts is an important process in the transport and enrichment of metals in magmatic and magmatic-hydrothermal systems, but the diffusivity of Ag, unlike other metals such as Cu, Mo, and W, is still unknown. In this study
Publikováno v:
Geochimica et Cosmochimica Acta. 290:16-26
Water diffusion is an important mechanism affecting magmatic water content, vapor bubble growth, and the dynamics of volcanic eruptions. Water diffusivity in silicate melts is dependent on temperature, pressure, H2O content and speciation, and melt c
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Publikováno v:
Carbon in Earth's Interior
Understanding the interactions between calcite and aqueous solutions is important when studying the deep carbon cycle. The present study investigates the solubility of calcite in salt-H2O fluids at 700 °C and 8 kbar. The investigated salts included
Publikováno v:
Earth and Planetary Science Letters. 522:40-47
Lunar volcanic glasses associated with mare basalt magmatism experienced significant degree of degassing, and to retrieve their initial water contents requires data of water diffusivity. We carried out diffusion experiments at 0.5 GPa and 1703–1903
Publikováno v:
Geochimica et Cosmochimica Acta. 259:129-143
The solubility of carbon in silicate melts (Fe-free MORB basalt, Fe-free andesite and Fe-free rhyolite) coexisting with graphite and a CO-CO2 fluid phase was measured to 3 GPa and 1500 °C. Experiments in the 0.2–0.5 GPa range were carried out in a
Publikováno v:
Contributions to Mineralogy and Petrology. 176
The temperature-dependent exchange of Ni and Mg between garnet and olivine in mantle peridotite is an important geothermometer for determining temperature variations in the upper mantle and the diamond potential of kimberlites. Existing calibrations
Publikováno v:
Physics and Chemistry of Minerals. 47
The study addresses the topic of fine-structural compression behaviour of solids. MgO / periclase and polyethylene / PE are studied as exemplary materials by volumetric and ultra-sound techniques at room temperature up to 1.5 GPa. The experiments con
Autor:
L.C. Baldwin, C. Ballhaus
Publikováno v:
Lithos. :447-454
Megacrystic sapphires (Fe-Ti-rich corundum) of up to 5 cm in size are well known from alkaline mafic rocks from intra-continental rift-related magmatic fields. There is no doubt that these sapphires represent xenocrysts that were trapped from their o