The surface textures of quartz sand grains from a Lower Triassic sandstone unit are almost identical to eolian sands from modern hot deserts, suggesting similar environments. This is the earliest example known of eolian surface textures unmodified by diagenesis; it shows how studies of surface textures of pre-Pleistocene sand grains may provide information about their depositional environments and subsequent diagenetic history.

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First page of Eolian transport textures on the surfaces of sand grains of Early Triassic age
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