The sulphides occur in a pillow-dyke transition zone. Transmitted and reflected light microscopy, XRD and probe analyses were used to decipher the complex paragenesis; minerals present include quartz, albite, sphene, chlorite, clays, actinolite, pyrite, epidote, sphalerite, chalcopyrite, galena, calcite and zeolites.-K.A.R.
|Original language||English (US)|
|Title of host publication||Initial Reports of the D.S.D.P.|
|Number of pages||20|
|Publication status||Published - 1985|
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)