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Dolomite Rock Grain Size

Pure dolomite sample were deformed at room temperature and under a variety of confining pressures 0 100MPa to examine the processes of grain size reduction. The dolomite is composed of gt 97 vol. dolomite with accessory quartz, calcite, tremolite, and muscovite and has been metamorphosed to amphibolite facies and subsequently annealed. At the hand sample scale, the rock is isotropic.

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