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粤西大王山动力变质带磁组构的构造意义
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作者 李建彪 《广东地质》 1999年第3期19-25,共7页
通过磁组构和岩石变形特征的研究并结合其他资料,推断出大王山动力变质带是在加里东晚期岩浆侵入成岩后,多期构造叠加作用的结果,识别出四期构造造变形:第一期为海西期的SWW→NEE构造滑脱作用;第二期为海西-印支期的NE向... 通过磁组构和岩石变形特征的研究并结合其他资料,推断出大王山动力变质带是在加里东晚期岩浆侵入成岩后,多期构造叠加作用的结果,识别出四期构造造变形:第一期为海西期的SWW→NEE构造滑脱作用;第二期为海西-印支期的NE向左行平移剪切作用;第三、四期分别为燕山早期和喜马拉雅期的NW→SE逆冲作用。 展开更多
关键词 磁级构 最小化率 断裂 动力变质带 大王山
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Preparation and mechanism of Fe_3O_4/Au core/shell super-paramagnetic microspheres 被引量:11
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作者 崔亚丽 胡道道 +1 位作者 房喻 马建标 《Science China Chemistry》 SCIE EI CAS 2001年第4期404-410,共7页
In the presence of Fe3O4 nano-particles, a new type of super-paramagnetic Fe3O4/Au microspheres with core/shell structures was prepared by reduction of Au3+ with hydroxylamine. The formation mechanism of the core/shel... In the presence of Fe3O4 nano-particles, a new type of super-paramagnetic Fe3O4/Au microspheres with core/shell structures was prepared by reduction of Au3+ with hydroxylamine. The formation mechanism of the core/shell microspheres was studied in some detail. It was shown that the formation of the complex microspheres can be divided into two periods, that is, surface reaction-controlled process and diffusion-controlled process. The relative time lasted by either process depends upon the amount of Fe3O4 added and the initial concentration of Au3+. XPS analysis revealed that along with increasing in coating amount, the strength of the characteristic peaks of Au increased, and the Auger peaks of Fe weakened and even disappeared. Size distribution analysis showed that the core/shell microspheres are of an average diameter of 180 nm, a little bit larger than those before coating. 展开更多
关键词 FE3O4 GOLD super-paramagnetic microspheres core/shell structure
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