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)|
|Number of pages||5|
|Issue number||2 EM|
|State||Published - Jan 1 1985|
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)