Environmental magnetic studies of lacustrine sediments

被引：40
作者：
Hu, SY
Deng, CL [1 ]
Appel, E
Verosub, KL
机构：
[1] Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[2] Inst Geol & Geophys, Beijing 100101, Peoples R China
[3] Univ Tubingen, Inst Geol, D-72076 Tubingen, Germany
[4] Univ Calif Davis, Dept Geol, Davis, CA 95616 USA
来源：
CHINESE SCIENCE BULLETIN | 2002年 / 47卷 / 07期
基金：
中国国家自然科学基金;
关键词：
rock magnetism; pateoclimate; paleoenvironment; lacustrine sediments;
D O I：
10.1360/02tb9141
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
In recent decades, environmental magnetism has become an important method for studying past global climatic and environmental changes. For an environmental magnetic study, it is important to understand the magnetic properties of various magnetic minerals in lacustrine sediments and the processes involved in the formation, transport, and preservation of these magnetic minerals. The magnetic response of lacustrine sediments to climatic change may vary widely from lake to lake. To reconstruct the processes contributing to paleoclimatic and paleoenvironmental change, it is, therefore, necessary to derive a complete understanding of the potential origin of the magnetic signal observed.
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收藏
页码：613 / U2
页数：6
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