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北京怀柔地区第四纪下限的综合标志
引用本文:李龙吟,陈华慧.北京怀柔地区第四纪下限的综合标志[J].地球科学,1992,17(6):631-637.
作者姓名:李龙吟  陈华慧
作者单位:中国地质大学 北京 (李龙吟),中国地质大学 北京(陈华慧)
摘    要:本文运用综合分析的方法,从岩性、古地磁、古生物、矿物及化学成分等方面,对北京怀柔地区HR88—1钻孔剖面进行了系统研究。认为HR88—1钻孔所揭露的新生代沉积物可划分为4个岩性段。第三与第四岩性段的界线即为N/Q界线,该界线位于孔深370m处。由于M/G界面位于358.5m深处,故确认N/Q界限时代约为2.50MaB.P.,将孔深370m以下的红色沉积物划归上新统,其上的杂色沉积物划归更新统。

关 键 词:第四纪  N/Q界限  综合标志  地层

COMPREHENSIVE CRITERIA FOR THE N/Q BOUNDARY IN HUAIROU AREA , BEIJING, CHINA
Li Longyin Chen Huahui.COMPREHENSIVE CRITERIA FOR THE N/Q BOUNDARY IN HUAIROU AREA , BEIJING, CHINA[J].Earth Science-Journal of China University of Geosciences,1992,17(6):631-637.
Authors:Li Longyin Chen Huahui
Abstract:The Cenozoic strata are fairly developed in Huairou area . Since 1988 a lot of useful work has been done and a good deal of information has been gained . In order to use the comprehensive method to identify the N/ Q boundary , we have systematically analyzed the lithology , heavy minerals , clay minerals ,pollen and spore , palaeomagnetic polarity of sediments in the borehole HR88 -l,many other materials are also concerned in this paper. The authors believe that the Cenozoic sediments uncovered in the borehole. HR88 - 1 can be divided into four members . The boundary between the third member and the fourth one is thought to be the N/Q boundary which lies at the depth of 370m from the ground surface . The geological time of the boundary is about 2.50MaB . P . because the bound of Matuyama reversed polarity zone and Gauss normal polarity zone is situated at 358.5m deep . According to this division , the red sediment under 370m deep belongs to Pliocene , and the sediment with multicolors above 370m deep belongs to Pleistocene .
Keywords:Beging  Quaternary  N/Q boundary  comprehensive criterion  
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