Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.
中新
积以细颗粒泥岩和砂岩为主，
明物源区较远 ，古流域坡度较小，搬运距离较
。
Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.
中新积以细颗粒泥岩和砂岩为主，明物源区较远 ，古流域坡度较小，搬运距离较。
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