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《Chinese Journal of Geophysics》 2002-06
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ROCK-MAGNETIC PROPERTIES OF HANNUOBA BASALT IN ZHANGBEI SECTION

TIAN LI-LI ZHU RI-XIANGPAN YONG-XIN (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101,China)  
By comprehensive rock-magnetic analyses of the Hannuoba basalt in the Zhangbei section, it has been shown that the main magnetic carriers of the twenty-one lava flows in this section are titano-magnetite, but the content of Ti is relatively high in some samples. Based on the anisotropy of magnetic susceptibility (AMS), the Hannuoba basalt was probably originated from two volcanoes that locate in the northeast and north-northwest directions, respectively which is consistent with the field observation. These results contribute to a better understanding of the eruption history of volcanoes and the deep Earth's interior processes in this region.
【Fund】: 国家自然科学基金项目 (4 983 40 0 1 );; 中国地震局构造物理开放实验室基金 (990 5 ) .
【CateGory Index】: P588.1
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