Abstract
HRTEM reveals a previously undescribed Fe-Ni-S-O layered mineral. The curved, rolled and wavy layers resemble serpentine minerals. It occurs in phyllosilicates in various ordered and disordered sequences.-K.A.R.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 67-71 |
| Number of pages | 5 |
| Journal | Norelco Reporter |
| Volume | 32 |
| Issue number | 2 EM |
| State | Published - 1985 |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences