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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

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Reference TypeJournal (article/letter/editorial)
TitleExperimental 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
JournalContributions to Mineralogy and Petrology
AuthorsMetz, PaulAuthor
Year1976Volume58
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00382182Search in ResearchGate
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Mindat Ref. ID74404Long-form Identifiermindat:1:5:74404:7
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Full ReferenceMetz, 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
Plain TextMetz, 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
In(1976) Contributions to Mineralogy and Petrology Vol. 58 (2) Springer Science and Business Media LLC

See Also

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

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
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
K�se, Hans -Rolf, Metz, Paul (1980) Experimental investigation of the metamorphism of siliceous dolomites. Contributions to Mineralogy and Petrology, 73 (2) 151-159 doi:10.1007/bf00371390
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
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
Suzuki, Kazuhiro (1977) Local equilibrium during the contact metamorphism of siliceous dolomites in Kasuga-mura, Gifu-ken, Japan. Contributions to Mineralogy and Petrology, 61 (1) 79-89 doi:10.1007/bf00375946
Widmark, E. Torbj�rn (1980) The reaction chlorite+dolomite=spinel+forsterite+calcite+carbon dioxide+water. Contributions to Mineralogy and Petrology, 72 (2) 175-179 doi:10.1007/bf00399477
Metz, Paul, Trommsdorff, Volkmar (1968) On phase equilibria in metamorphosed siliceous dolomites. Contributions to Mineralogy and Petrology, 18 (4) 305-309 doi:10.1007/bf00399692
Puhan, D. (1988) Reverse age relations of talc and tremolite deduced from reaction textures in metamorphosed siliceous dolomites of the southern Damara Orogen (Namibia) Contributions to Mineralogy and Petrology, 98 (1) 24-27 doi:10.1007/bf00371905
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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