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河南邙岭塬黄土地层
引用本文:王书兵,蒋复初,吴锡浩,田国强,赵志中,刘萪,王志明. 河南邙岭塬黄土地层[J]. 地质力学学报, 2001, 7(4): 309-314
作者姓名:王书兵  蒋复初  吴锡浩  田国强  赵志中  刘萪  王志明
作者单位:1. 中国地质科学院地质力学研究所, 北京 100081;
基金项目:国家自然科学基金(49972060);国家重点基础研究专项经费资助项目(G1999043401)
摘    要:通过河南邙岭塬北缘中部,孟津扣马黄土剖面野外观测及室内磁化率研究,剖面共发育11层(S1~11)以上黄土-古土壤序列,各层古土壤清晰;但第二层(S2)的磁化率值相对较低,而且与第三层(S3)间所夹黄土层非常薄,显示异常特征。古地磁测试结果揭示,B/M界限在深度38.9m处,位于L8的底部。松山负极性时晚期,记录了两段正极性。 

关 键 词:黄土   邙岭塬   河南
文章编号:1006-6616(2001)04-0309-06
收稿时间:2001-08-12
修稿时间:2001-08-12

LOESS STRATIGRAPHY OF MANGLING IN HENAN PROVINCE
WANG Shu-bing,JIANG Fu-chu,WU Xi-hao,TIAN Guo-qiang,ZHAO Zhi-zhong,LIU Ke and WANG Zhi-ming. LOESS STRATIGRAPHY OF MANGLING IN HENAN PROVINCE[J]. Journal of Geomechanics, 2001, 7(4): 309-314
Authors:WANG Shu-bing  JIANG Fu-chu  WU Xi-hao  TIAN Guo-qiang  ZHAO Zhi-zhong  LIU Ke  WANG Zhi-ming
Affiliation:1. Institute of Geomechanics, CAGS, Beijing 100081, China;2. Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, Shaanxi 710054, China;3. Electric Power Construction Co., Ltd., Zhejiang Hangzhou 310051, China
Abstract:In this paper,Kouma profile,located in Mengjin,Henan north of middle Mangling Plateau Form has been studied.This profile contains S11 and upwands loess-paleosol each loess and paleosol are clear.The magnetic susceptibility curve shows that the susceptibility value of S2 is lower than the others,while the thickness of L3 is very thin,showing abnovmal character.Palaeomagnetic stratigraphy shows that the depth of the boundary between Brunhes normal polarity chron and Matuyama reversed one is 38.9 meters,which located at the lower part of L8.Furthermore,two normal polarity intervals are revealed in the late Matuyama reversed polarity chron.
Keywords:loess  Mangling Plateau Form  Henan
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