PECORAITE, NI6SI4O10(OH)8, NICKEL ANALOG OF CLINOCHRYSOTILE FORMED IN WOLF CREEK METEORITE

被引：40
作者：
FAUST, GT
FAHEY, JJ
MASON, B
DWORNIK, EJ
机构：
[1] U.S. Geological Survey, Washington
[2] U.S. National Museum, Washington
来源：
SCIENCE | 1969年 / 165卷 / 3888期
关键词：
D O I：
10.1126/science.165.3888.59
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Pecoraite is a new phase in the natural system H2O-NiO-MgO- SiO2, the nickel analog of clinochrysotile. It occurs in cracks in the Wolf Creek meteorite in Australia where it was formed under hydrothermal conditions. Particles of pecoraite are very small curved plates which have begun to coil; some have achieved spiral form.
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页码：59 / &
相关论文
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