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岱海湖泊沉积岩芯高分辨率磁性测量——U型槽与常规方法之比较
引用本文:朱艳明, 于永涛, 周力平, 薛滨, 吴艳宏, 强小科. 岱海湖泊沉积岩芯高分辨率磁性测量——U型槽与常规方法之比较[J]. 第四纪研究, 2007, 27(6): 983-988.
作者姓名:朱艳明  于永涛  周力平  薛滨  吴艳宏  强小科
作者单位:1. 北京大学地理学院地表过程分析与模拟教育部重点实验室, 北京10087; 2. 中国科学院南京地理与湖泊研究所湖泊沉积与环境重点实验室, 南京 210008; 3. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710075
摘    要:对岱海西南部湖滨地区(40°32.127′N,112°37.802′E)钻取的一根长79.16m的高取芯率(98.8%)沉积岩芯(DH06A)进行了高分辨率的湖泊沉积物磁学性质测量。对U型槽法和常规散样方法得到的磁化率和非磁滞剩余磁化强度测量结果进行了系统的比较。

关 键 词:岱海   U型槽   磁化率   ARM   湖泊沉积物
文章编号:1001-7410(2007)06-983-06
收稿时间:2007-06-18
修稿时间:2007-07-25

HIGH-RESOLUTION MAGNETIC MEASUREMENTS ON A LAKE SEDIMENT CORE FROM DAIHAI LAKE: COMPARISON BETWEEN U-CHANNEL AND DISCRETE SAMPLE METHODS
Zhu Yanming, Yu Yongtao, Zhou Liping, Xue Bin, Wu Yanhong, Qiang Xiaoke. HIGH-RESOLUTION MAGNETIC MEASUREMENTS ON A LAKE SEDIMENT CORE FROM DAIHAI LAKE:COMPARISON BETWEEN U-CHANNEL AND DISCRETE SAMPLE METHODS[J]. Quaternary Sciences, 2007, 27(6): 983-988.
Authors:Zhu Yanming  Yu Yongtao  Zhou Liping  Xue Bin  Wu Yanhong  Qiang Xiaoke
Affiliation:1. Department of Geography, Laboratory for Earth Surface Processes, Peking University, Beijing 100871;; 2. Key Laboratory of Lake Sedimentation and Environment,Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences, Nanjing 210008;; 3. State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences, Xi′an 710075
Abstract:High-resolution magnetic measurement on lake sediments from arid and semi-arid regions is an important means of characterizing paleoenvironmental changes. Previous research has shown that the Daihai Lake, an inland graben-type basin in Inner Mongolia, China, contains rich information about the evolution of paleomonsoons. Here we present results of high-resolution magnetic measurements of the lake sediments from a 79.16m core(DH06A), drilled at the southeast littoral area of the Daihai Lake(40°32.127′N, 112°37.802′E).
Keywords:Daihai Lake   U-channel   magnetic susceptibility parameters   ARM   lake sediments
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