A preliminary study of the magnetostratigraphic column suggests that the upper and lower parts separated at a depth of 386. 0 m from the surface belong to the Gauss normal polarity chron and the Gilbert reverse polarity chron respectively.

 
  • 磁性地層初步研究表明;以距頂深度386.;0m處為界;以上為高斯正向極性帶;以下為吉爾伯特反向極性帶。
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