在这一廊带中，由南向北其下马岭组沉积厚度和斑脱岩的层数逐渐增大。
From the south to the north, both the thickness of the third member of the Xiamaling Fm. and the number of K-bentonite layers increase gradually.
在这一廊带中，由南向北其下马岭组沉积厚度和斑脱岩的层数逐渐增大。
From the south to the north, both the thickness of the third member of the Xiamaling Fm. and the number of K-bentonite layers increase gradually.
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