Pyrrhotite-troilite intergrowth from Luikonlahti copper deposit, eastern Finland

A homoaxial intergrowth of troilite with iron-deficient pyrrhotite, Fe0.921S, is described. X-ray single crystal study of the pyrrhotite component points to a superstructure with c = 11 C and apparently to an orthorhombic symmetry. The intergrowth occurs on fissure walls in serpentinite rock as euhe...

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Bibliographic Details
Main Author: A. Vorma
Format: Article
Language:English
Published: Geological Society of Finland 1970-12-01
Series:Bulletin of the Geological Society of Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume42/sgs_bt_042_pages_003_012.pdf
Description
Summary:A homoaxial intergrowth of troilite with iron-deficient pyrrhotite, Fe0.921S, is described. X-ray single crystal study of the pyrrhotite component points to a superstructure with c = 11 C and apparently to an orthorhombic symmetry. The intergrowth occurs on fissure walls in serpentinite rock as euhedral long-prismatic crystals; it apparently formed at a very low temperature. Possibly a simultaneous crystallization of troilite and iron-deficient pyrrhotite took place.
ISSN:0367-5211
1799-4632