| Abstract: | 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. |
| Genre: | Article |
| ProdID: | 70011502 |
| Citation Author: | Faust, G. T.; Fahey, J. J.; Mason, B.; Dwornik, E. J. |
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| Citation End Page: | 60 |
| Citation Issue: | 3888 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 2 |
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| Citation Search Results Text: | Pecoraite, Ni6Si4O10(OH)8, nickel analog of clinochrysotile, formed in the wolf creek meteorite; 1969; Article; Journal; Science; Faust, G. T.; Fahey, J. J.; Mason, B.; Dwornik, E. J. |
| Citation Start Page: | 59 |
| Citation Volume: | 165 |
| Citation Year: | 1969 |
| Type: | citation/reference |
| Text: | Pecoraite, Ni6Si4O10(OH)8, nickel analog of clinochrysotile, formed in the wolf creek meteorite; 1969; Article; Journal; Science; Faust, G. T.; Fahey, J. J.; Mason, B.; Dwornik, E. J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1969 00:00 -0600 |
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