Browsing ELibrary by Author "Xu Z."
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Browsing ELibrary by Author "Xu Z."
Now showing items 1-8 of 8
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Jenkins D.M.; Sherriff B.L.; Cramer J.; Xu Z. (1997)A series of aluminous tremolites was synthesized at 800-850 8C and 6-13 kbar along the join Ca1.8Mg5.2Si8O22(OH)2-Ca1.8(Mg4.2Al)(AlSi7)O22(OH)2 by means of the Mg-Tscher- maks substitution. Although the amphibole yields ...
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Behrens H.; Zhang Y.; Xu Z. (2004)The diffusion of water in dacitic and andesitic melts was investigated at temperatures of 1458 to 1858 K and pressures between 0.5 and 1.5 GPa using the diffusion couple technique. Pairs of nominally dry glasses and hydrous ...
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Zhang Y.; Xu Z.; Behrens H. (2000)The hydrous species geospeedometer is based on the homogeneous interconversion reaction between molecular H2O species and OH species in silicate melts and glasses. Here we report new data for the calibration of the ...
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Zhang Y.; Xu Z. (2003)Large quantities of methane hydrate are present in marine sediment. When methane hydrate is exposed or released to seawater, it dissolves in seawater or dissociates into methane gas and water. There was some confusion in ...
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Xu Z.; Stebbins J.F. (1998)17O solid state nuclear magnetic resonance (NMR) was applied to study the oxygen exchange kinetics between framework oxygens and oxygens in the channel waters in the zeolite mineral stilbite. We have shown that framework ...
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Xu Z.; Zhang Y. (2002)We apply a geospeedometer previously developed in this lab to investigate cooling rate profiles of rhyolitic samples initially held at 720-750°C and quenched in water, liquid nitrogen, and air. For quench of mm-size samples ...
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Mériaux A.-S.; Tapponnier P.; Ryerson F.J.; Van der Woerd J.; Finkel R.C.; Caffee M.W.; Xu X.; Xu Z. (2004)To better constrain the ongoing rates of deformation in northern Tibet, the ages of fluvial and glacial geomorphic markers left-laterally displaced by the Altyn Tagh Fault have been determined by radiocarbon and 10Be-26Al ...
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Greenwood B.; Xu Z. (2001)Laboratory simulation of wave shoaling over a medium sand bed (mean size=250μm) for a range of wave conditions (a natural spectrum, symmetrical and asymmetrical wave groups) showed that a distinct horizontal fractionation ...
Now showing items 1-8 of 8
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