Ion microprobe U-Th-Pb dating of Shergotty phosphates

Physics

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Scientific paper

We report ion microprobe U-Th-Pb dating of Shergotty phosphates by means of the SHRIMP instrumention recently installed at Hiroshima University, Japan. Ten analyses of whitlockite (merrillite) and three analyses of apatite indicate a 238U/206Pb isochron age of 225 ± 200 Ma and a Tera-Wasserburg concordia constrained linear 3-D isochron age of 217 ± 110 Ma in the 238U/206Pb-207Pb/206Pb-204Pb/206Pb diagram. These ages agree well with the 232Th-208Pb age of 189 ± 83 Ma, suggesting primary crystallization or a shock metamorphic event defined the formation age of the phosphate minerals. The average of the later two ages, 204 ± 68 Ma, is consistent with the previously published Rb-Sr age of 165 ± 11 Ma and U-Th-Pb age of ~200 Ma. These show marginal agreement with the 40Ar-39Ar age of 254 ± 10 Ma, but are significantly different from the Sm-Nd age of 360 ± 16 Ma. Taking into account the closure temperature of the U-Pb system in apatite, we suggest the time when a temperature of about 900 oC was last experienced by Shergotty is 204 ± 68 Ma.

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