CAJ | 학술논문

河南荥阳孤柏嘴黄土剖面古地磁研究表明B/M界线位于S8上部(剖面119.4m处)，80多米厚的马兰黄土中发现4层弱发育的古土壤。古地磁研究结果为邙山黄土地层的划分提供了重要的时间控制，为南水北调中线工程穿黄工程的设计提供了重要的基础，并且表明该剖面在提取黄土沉积所记录的高分辨率的过去全球变化信息的研究中具有重要意义。
하남형양고백취황토부면고지자연구표명B/M계선위우S8상부(부면119.4m처)，80다미후적마란황토중발현4층약발육적고토양。고지자연구결과위망산황토지층적화분제공료중요적시간공제，위남수북조중선공정천황공정적설계제공료중요적기출，병차표명해부면재제취황토침적소기록적고분변솔적과거전구변화신식적연구중구유중요의의。
Palaeomagnetism study in Gubaizui loess section in Xingyang,Henan Province indicates that B/M boundary locates in upper part of S8 at 119.4 m depth of Gubaizui loess section. Four layers not mature paleosoil embedded in Malan loess have been found. This result provides an important time control over the Mangshan loess and gives the basic information for the design of the project of crossing the Yellow River in the project of driving waters from south to north. For the more it also shows that the section is quite good for study of past global changes with high resolution.