Detrital zircon–apatite fingerprinting challenges glacial transport of Stonehenge’s megaliths
Anthony J. I. Clarke, Christopher L. Kirkland
原始摘要（英文原文）· Original abstract
Salisbury Plain detrital zircon ages align with southern British rocks from the London Basin, indicating local sedimentary recycling without glaciogenic evidence, negating glacial transport of the Stonehenge blocks, according to detrital zircon and apatite U-Pb isotopic fingerprinting of stream sediments across the Salisbury Plain.