The low-high quartz and quartz-coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO2component on the low quartz-coesite transition

Author:

Mirwald Peter W.,Massonne H.-J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference43 articles.

1. Quartz ⇌ coesite transition and the comparative friction measurements in piston-cylinder apparatus using talc-alsimag-glass (TAG) and NaC1 high-pressure cells;Akella;Neues Jahrb. Mineral. Monatsh.,1979

2. Melting of gold, silver and copper-Proposal for a new high-pressure calibration scale;Akella;J. Geophys. Res.,1971

3. Isothermal compression of stishovite and coesite up to 85 kilobars at room temperature by X-ray diffraction;Bassett;Phys. Earth Planet. Interiors,1970

4. Shearing squeezer experiments with quartz and coesite;Bell;Carnegie Inst. Wash. Yearb.,1965

5. Temperature-pressure plane for albite composition;Birch;Amer. J. Sci.,1960

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