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Lüttge, Andreas, Metz, Paul (1993) Mechanism and kinetics of the reaction: 1 dolomite + 2 quartz = 1 diopside + 2 CO2: a comparison of rock-sample and of powder experiments. Contributions to Mineralogy and Petrology, 115 (2) 155-164 doi:10.1007/bf00321217

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Reference TypeJournal (article/letter/editorial)
TitleMechanism and kinetics of the reaction: 1 dolomite + 2 quartz = 1 diopside + 2 CO2: a comparison of rock-sample and of powder experiments
JournalContributions to Mineralogy and Petrology
AuthorsLüttge, AndreasAuthor
Metz, PaulAuthor
Year1993 (November)Volume115
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00321217Search in ResearchGate
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Mindat Ref. ID76992Long-form Identifiermindat:1:5:76992:1
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Full ReferenceLüttge, Andreas, Metz, Paul (1993) Mechanism and kinetics of the reaction: 1 dolomite + 2 quartz = 1 diopside + 2 CO2: a comparison of rock-sample and of powder experiments. Contributions to Mineralogy and Petrology, 115 (2) 155-164 doi:10.1007/bf00321217
Plain TextLüttge, Andreas, Metz, Paul (1993) Mechanism and kinetics of the reaction: 1 dolomite + 2 quartz = 1 diopside + 2 CO2: a comparison of rock-sample and of powder experiments. Contributions to Mineralogy and Petrology, 115 (2) 155-164 doi:10.1007/bf00321217
In(1993, November) Contributions to Mineralogy and Petrology Vol. 115 (2) Springer Science and Business Media LLC

See Also

These are possibly similar items as determined by title/reference text matching only.

Lüttge, A., Metz, P. (1991) Mechanism and kinetics of the reaction 1 dolomite + 2 quartz = 1 diopside + 2 CO2 investigated by powder experiments. The Canadian Mineralogist, 29 (4) 803-821
Dachs, Edgar, Metz, Paul (1988) The mechanism of the reaction 1 tremolite+3 calcite+2 quartz =5 diopside+3 CO2+1 H2O: results of powder experiments. Contributions to Mineralogy and Petrology, 100 (4) 542-551 doi:10.1007/bf00371382
Heinrich, Wilhelm, Metz, Paul, Gottschalk, Matthias (1989) Experimental investigation of the kinetics of the reaction 1 tremolite+11 dolomite?8 forsterite+13 calcite+9 CO2+1 H2O. Contributions to Mineralogy and Petrology, 102 (2) 163-173 doi:10.1007/bf00375338
Heinrich, Wilhelm, Metz, Paul, Bayh, Werner (1986) Experimental investigation of the mechanism of the reaction: 1 tremolite+11 dolomite ? 8 forsterite+13 calcite+9 CO2+1H2O. Contributions to Mineralogy and Petrology, 93 (2) 215-221 doi:10.1007/bf00371323
Luth, Robert W. (1995) Experimental determination of the reaction dolomite + 2 coesite = diopside + 2 CO 2 to 6 GPa. Contributions to Mineralogy and Petrology, 122 (1) 152-158 doi:10.1007/s004100050118
Metz, Paul (1976) Experimental investigation of the metamorphism of siliceous dolomites III. Equilibrium data for the reaction: 1 Tremolite + 11 dolomite ? 8 forsterite + 13 calcite + 9 CO2 +1H2O for the total pressures of 3,000 and 5,000 bars. Contributions to Mineralogy and Petrology, 58 (2) 137-148 doi:10.1007/bf00382182
Puhan, D. (1995) Metamorphic evolution of the assemblage tremolite + talc + calcite + dolomite + quartz within a sample of siliceous dolomite from the southern Damara Orogen (Namibia) Contributions to Mineralogy and Petrology, 120 (2) 180-185 doi:10.1007/bf00287115
Puhan, D. (1995) Metamorphic evolution of the assemblage tremolite + talc + calcite + dolomite + quartz within a sample of siliceous dolomite from the southern Damara Orogen (Namibia) Contributions to Mineralogy and Petrology, 120 (2) 180-185 doi:10.1007/s004100050068
Jenkins, David M. (2011) The transition from blueschist to greenschist facies modeled by the reaction glaucophane + 2 diopside + 2 quartz = tremolite + 2 albite. Contributions to Mineralogy and Petrology, 162 (4) 725-738 doi:10.1007/s00410-011-0621-8
Gasparik, Tibor (1996) Melting experiments on the enstatite-diopside join at 70-224 kbar, including the melting of diopside. Contributions to Mineralogy and Petrology, 124 (2) 139-153 doi:10.1007/s004100050181
Heaney, Peter J. (1993) A proposed mechanism for the growth of chalcedony. Contributions to Mineralogy and Petrology, 115 (1) 66-74 doi:10.1007/bf00712979
 
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