Magnetic Properties of Late Pleistocene Sediments in Core DSHoft-com:office:smarttags" />-1C from Northern South China Sea and Their Environment Significanceoft-com:office:office" />

• 责任者：Luo Yi (School of Ocean Sciences ; China University of Geosciences ; Beijing 100083 ; China) ; Su Xin
• 刊名：Geoscience
• 出版年：2010
• 卷期：24(3)
• 关键词：Upper Pleistocene ; Holocene ; 磁性组构 ; magnetic fabric ; 南海 ; South China Sea
• 页码：p.521-527
• 图表：5 illus., 1 table, 28 refs.
• 分类号：1400
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

A study of magnetic properties of sediments at the piston core DSHoft-com:office:smarttags" />-1C from deep sea area of Dongsha, the South China Sea was carried out.  According to magnetic properties obtained, it was inferred that sediments from the core contained very rare magnetic minerals.Lowest values of magnetic properties (χ, NRM and SIRM) were observed in the intervals of Unit II, where turbidity layers containing abundant calcareous foraminifera shells occurred, indicating the dilution of carbonate in these sediment layers.  oft-com:office:office" />