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

doi:10.2973/dsdp.proc.83.110.1985

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 journal › Article › peer-review

49 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 language	English (US)
Pages (from-to)	263-282
Number of pages	20
Journal	Initial Reports of the D.S.D.P.
Volume	83
DOIs	https://doi.org/10.2973/dsdp.proc.83.110.1985
State	Published - 1985
Externally published	Yes

ASJC Scopus subject areas

General Environmental Science
General Earth and Planetary Sciences

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10.2973/dsdp.proc.83.110.1985

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

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.",

author = "J. Honnorez and Alt, \{J. C.\} and B. Honnorez-Guerstein and C. Laverne and K. Muehlenbachs and J. Ruiz and Saltzman, \{E. S.\}",

year = "1985",

doi = "10.2973/dsdp.proc.83.110.1985",

language = "English (US)",

volume = "83",

pages = "263--282",

journal = "Initial Reports of the D.S.D.P.",

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TY - JOUR

T1 - Stockwork-like sulfide mineralization in young oceanic crust

T2 - Deep Sea Drilling Project hole 504B.

AU - Honnorez, J.

AU - Alt, J. C.

AU - Honnorez-Guerstein, B.

AU - Laverne, C.

AU - Muehlenbachs, K.

AU - Ruiz, J.

AU - Saltzman, E. S.

PY - 1985

Y1 - 1985

N2 - 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.

AB - 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.

UR - https://www.scopus.com/pages/publications/0022007748

UR - https://www.scopus.com/pages/publications/0022007748#tab=citedBy

U2 - 10.2973/dsdp.proc.83.110.1985

DO - 10.2973/dsdp.proc.83.110.1985

M3 - Article

AN - SCOPUS:0022007748

VL - 83

SP - 263

EP - 282

JO - Initial Reports of the D.S.D.P.

JF - Initial Reports of the D.S.D.P.

ER -

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

Abstract

ASJC Scopus subject areas

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