Magnetic Fabric Characteristics and Implications for Its Origin of “Wushan Loess”oft-com:office:office" />

• 责任者：Zhang Yufen (Institute of Geophysics & Geomatics ; China University of Geosciences ; Wuhan 430074 ; China) ; Li Chang’an
• 刊名：Earth Science
• 出版年：2010
• 卷期：35(5)
• 关键词：黄土 ; loess ; 磁性组构 ; magnetic fabric ; 长江 ; Yangtze River
• 页码：p.885-890
• 图表：3 illus., 1 table, 21 refs.
• 分类号：1400
• issnNo：ISSN1000-2383
• isbnNo：CN42-1233/P

In this paper, the present the magnetic fabric and magnetic susceptibility characters of one newly found “Wushan Loess” Section, which was also compared with the modern oft-com:office:smarttags" />Yangtze River sediments and aeolian loess and “Sand-Dune” sediments distributed at the Middle Yangtze River. The results are as follows: 1) the κ, P, F, L, E values of the “Wushan Loess” are close to those of the aeolian loess and “Sand-Dune” sediments; 2) shown on the F-L graph, data of the “Wushan Loess” converge upon the origin of coordinates, similar to the aeolian loess and “Sand-Dune” sediments distributed at the Middle Yangtze River; and 3) maximum magnetic principal axis of the “Wushan Loess” is similar to that of the aeolian loess and “Sand-Dune” sediments distributed at the Middle Yangtze River.  oft-com:office:office" />