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, Joaquin Ruiz, E. S. Saltzman

Research output: Chapter in Book/Report/Conference proceedingChapter

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)
Title of host publicationInitial Reports of the D.S.D.P.
Pages263-282
Number of pages20
Volume83
Publication statusPublished - 1985
Externally publishedYes

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ASJC Scopus subject areas

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

Cite this

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. In Initial Reports of the D.S.D.P. (Vol. 83, pp. 263-282)