Stockwork-like sulfide mineralization in young oceanic crust: Deep Sea Drilling Project hole 504B.

J. Honnorez, J. C. Alt, B. Honnorez-Guerstein, C. Laverne, K. Muehlenbachs, J. Ruiz, E. S. Saltzman

Research output: Contribution to journalArticle

44 Scopus citations

Abstract

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 languageEnglish (US)
Pages (from-to)263-282
Number of pages20
JournalInitial Reports of the D.S.D.P.
Volume83
DOIs
StatePublished - 1985

ASJC Scopus subject areas

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

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    Honnorez, J., Alt, J. C., Honnorez-Guerstein, B., Laverne, C., Muehlenbachs, K., Ruiz, J., & Saltzman, E. S. (1985). Stockwork-like sulfide mineralization in young oceanic crust: Deep Sea Drilling Project hole 504B. Initial Reports of the D.S.D.P., 83, 263-282. https://doi.org/10.2973/dsdp.proc.83.110.1985