2006
DOI: 10.2465/jmps.jmps.060106
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Structural state of plagioclase from the Kobe CK chondrite: Implications for the thermal history of the CK parent body

Abstract: We determined the structural state of six plagioclase crystals from the Kobe meteorite by measuring the separation between the 13 1 and 131 X ray diffraction peaks (Δ131 parameter) using a Gandolfi camera. The formation temperature of each plagioclase crystal was then estimated by plotting the Δ131 parameter on the relation diagram between the Δ131 parameters and temperatures of plagioclase synthesis, as proposed by Smith (1972). Three of the crystals record temperatures of just under 700 °C, while the other t… Show more

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