Abstract
To examine whether the long‐term averaged solar flare Ne is "planetary" type, as observed in contemporary solar flares, we have studied etched feldspar separates of several lunar soils and three samples from different depths of two well‐documented lunar rocks. Our results of noble gas elemental and isotopic ratios suggest that the long‐term average solar flare Ne composition is more similar to "solar" type than the "planetary" type.
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