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  • In this paper, the stable isotopic stratigraphies of two size fractions (>38 and
  • of variations seen in these stratigraphies, the AA. have documented the major isotopic signal carriers in INMD box 111 No. 6, and how their proportions vary.
  • 1991
  • The application of oxygen isotopic stratigraphy appears to be a useful technique in the chronostratigraphy of subaerial loess sequences, but further data and comparisons are needed particularly in the case of older stages and loess cycles.
  • 1991