梅里休伊特 (Merrihueite) 是一种从中东马达拉斯的地铁酸盐中获得的性-铁磁性酸盐
概括
梅里胡伊特 (Merrihueite) 是一种在梅索-马达拉斯 (Mezö-Madaras) 合金矿石中发现的新矿物质,是一种酸铁磁酸盐. 它的特性与osmiilite相似,表明这种类型的新矿物.
科学领域:
- 矿物学是什么?矿物学是什么?
- 宇宙化学 宇宙化学
- 石化学 石化学是一门学科.
背景情况:
- 石为早期太阳系过程提供了洞察力.
- 孔德里特是原始的石,含有孔德鲁,这是早期形成的组成部分.
研究的目的:
- 为了描述一种新发现的矿物质 - - 矿石 (merrihueite),这种矿物是在矿石中发现的.
- 为了确定矿物的化学成分,物理性质和结构关系.
主要方法:
- 化学分析以确定大致成分: (K,Na) () (二) (铁) () (五) (锡) (十二) (O) (三十).
- 光学显微镜测量折射率 (1.5591.592) 和双折射率.
- 用X射线粉碎衍射来比较已知矿物质,如 osumilite.
主要成果:
- 在梅索-马达拉斯石的柱体中发现了梅里胡伊特,它与奥利文,氧化和铁一起存在.
- 测量了它的光学特性 (折射率,双折射率).
- X射线数据显示与osmilite和合成K2Mg5Si12O30有很强的相似性.
结论:
- 梅里休伊特被归类为一种新的矿物种.
- 它被解释为一种酸铁磁酸盐,属于酸铁酸盐组.
- 这种矿物质以石学家克雷格·M·梅里休 (Craig M. Merrihue) 的名字命名.
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