期刊
AMERICAN MINERALOGIST
卷 94, 期 7, 页码 1059-1062出版社
MINERALOGICAL SOC AMER
DOI: 10.2138/am.2009.3216
关键词
Quartz; lattice strain; residual stress; Laue microdiffraction
资金
- U.S. Department of Energy [DE-AC02-05CH11231]
- DOE [DE-FG02-05ER15637]
- NSF [EAR 0836402]
Residual elastic strain in naturally deformed, quartz-containing rocks can be measured quantitatively in a petrographic thin section with high spatial resolution using Laue microdiffraction with white synchrotron X-rays. The measurements with a resolution of 1 mu m allow the quantitative determination of the deviatoric strain tensor as a function of position within the crystal investigated. The observed equivalent strain values of 800-1200 microstrains represent a lower bound of the actual preserved residual strain in the rock, since the stress component perpendicular to the cut sample surface plane is released. The measured equivalent strain translates into an equivalent stress ill the order of similar to 50 MPa.
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