A new layered mineral from the Mighei carbonaceous chondrite.

K. Tomeoka, P R Buseck

Research output: Contribution to journalArticle

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 languageEnglish (US)
Pages (from-to)67-71
Number of pages5
JournalNorelco Reporter
Volume32
Issue number2 EM
StatePublished - Jan 1 1985

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

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