A thermoluminescence study of experimentally shock-loaded oligoclase and bytownite

Details A thermoluminescence study of experimentally shock-loaded oligoclase and bytownite A thermoluminescence study of experimentally shock-loaded oligoclase and bytownite

Nov 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986jgr....91..263h&link_type=abstract

(Lunar and Planetary Institute, NASA, AAS, et al., Lunar and Planetary Science Conference, 17th, Houston, TX, Mar. 17-21, 1986)

Physics

6

Feldspars, Meteoritic Composition, Mineralogy, Planetary Surfaces, Shock Loads, Thermoluminescence, Earth Crust, Metamorphism (Geology)

Scientific paper

The thermoluminescence (TL) properties of a terrestrial oligoclase and a bytownite shock-loaded to pressures of 10.5-45 GPa are measured. Glow curves and TL sensitivity levels for the oligoclase and bytownite samples are presented and analyzed; it is detected that shock causes a decrease in the TL sensitivity and changes the shape of the glow curve. The causes of the decrease in TL sensitivity and peak temperature and width variations are examined. Shock-induced disordering of the Al, Si chain, and ordinary chondrite shocks are studied.

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