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库水硼镁石(Mg_2B_6O_(11)·15 H_2O Kurnakovite)是一种少见的镁的含水硼酸盐矿物。首次发现于苏联哈萨克斯坦,第二次发现是在美国的加州,而Heinrich将其误认为是多水硼镁石(Mg_2 B_6O_(11)·15 H_2O inderite)了,因此造成了在名称上英文和俄文之间的混乱。后来沙勒和姆罗斯把这个问题澄清了,指出库水硼镁石和多水硼镁石是一对同质多象变体,前者是三斜的,后者是单斜的。本工作中所用样品系谢先德同志提供,曾由谢先德等做过详细的矿物学和结晶学研究。本文作者又重新测定了晶胞参数: a=8.36±0.02 A,b=10.72±0.02 A,c=
Cu-boehmite (Mg_2B_6O_ (11) .15H_2O Kurnakovite) is a rare magnesium hydrate borate mineral. First discovered in the Soviet Union of Kazakhstan, the second discovery was in California of the United States, and Heinrich misidentified it as borate (Mg_2B_6O_ (11) .15H_2O inderite), resulting in the name of the English and Confusion between Russians. Later, Shalom and Mouros clarified this question, pointing out that the kibuocite and doxorubicin are a pair of homogeneous multimodal variants, the former being triclinic and the latter being monoclinic. The samples used in this work are provided by Comrade Xie Xiande, who conducted detailed mineralogy and crystallography studies by Xie Xiande et al. The authors again re-measured the unit cell parameters: a = 8.36 ± 0.02 A, b = 10.72 ± 0.02 A, c =