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东菲律宾海柱样沉积物的磁性特征
引用本文:孟庆勇,李安春,靳宁,徐兆凯,刘建国.东菲律宾海柱样沉积物的磁性特征[J].海洋地质与第四纪地质,2006,26(3):57-63.
作者姓名:孟庆勇  李安春  靳宁  徐兆凯  刘建国
作者单位:1. 中国科学院,海洋研究所,青岛,266071;中国科学院,研究生院,北京,100039
2. 中国科学院,海洋研究所,青岛,266071
基金项目:国家自然科学基金项目(40576032)
摘    要:对东菲律宾海帕里西维拉海盆西侧F090102柱样进行了系统的古地磁和岩石磁学研究,测量了天然剩磁倾角、磁化率、饱和等温剩磁、非磁滞剩磁、-T曲线等磁学参数,进行了磁性地层的划分对比,识别出松山反极性时内的贾拉米洛和奥都维正极性亚时。对磁学参数及其有关比值的研究发现,岩心磁性矿物以低矫顽力磁铁矿为主,可能含有一定的钛磁铁矿。磁性矿物主要是陆源碎屑成因,岩心底段受到海底火山作用的影响。根据磁学参数随深度的变化将岩心分为3段,各段反映了沉积环境和古气候的变化。

关 键 词:柱样沉积物  磁性特征  东菲律宾海
文章编号:0256-1492(2006)03-0057-07
修稿时间:2005年12月23

MAGNETOSTRATIGRAPHIC AND MAGNETIC PROPERTIES OF MARINE SEDIMENTS FROM THE EAST PHILIPPINE SEA
MENG Qing-yong,LI An-chun,JIN Ning,XU Zhao-kai,LIU Jian-guo.MAGNETOSTRATIGRAPHIC AND MAGNETIC PROPERTIES OF MARINE SEDIMENTS FROM THE EAST PHILIPPINE SEA[J].Marine Geology & Quaternary Geology,2006,26(3):57-63.
Authors:MENG Qing-yong  LI An-chun  JIN Ning  XU Zhao-kai  LIU Jian-guo
Abstract:A detailed magnetic analysis has been done on core F090102 from the East Philippine Sea,and the following magnetic parameters were measured: susceptibility(X_1),anhysteretic remnant magnetization(ARM),saturation isothermal remnant magnetization(SIRM),IRM_-300 mT(induced in a field of-300mT)and typical temperature dependence of magnetic susceptibility curves(X_1-T).Analyses of magnetic parameters demonstrated that magnetic minerals in the sequence are dominated by low-coercivity ferromagnetic minerals with subordinate high-coercivity antiferromagnetic minerals and are characterized by magnetite(probably including some titanomagnetites).The results show that the rock-magnetic parameters well correspond to the paleoclimatic variations and sedimentary environmental changes.And a magnetostratigraphic record was obtained.The Bruhnes-Matuyama reversal,the Jaramillo event as well as the Olduvai event during the Matuyama period were identified.
Keywords:core sediments  magnetic properties  East Philippine Sea
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