Growth history of a diffusely venting sulfide structure from the Juan de Fuca Ridge: A petrological and geochemical study

Author:

Kristall Brian1,Kelley Deborah S.1,Hannington Mark D.2,Delaney John R.1

Affiliation:

1. School of Oceanography and Astrobiology Program; University of Washington; Box 357940,; Seattle; Washington; 98195; USA

2. Department of Earth Sciences; University of Ottawa; 140 Louis Pasteur,; Ottawa, Ontario; Canada; K1N 6N5

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference79 articles.

1. Hydrothermally precipitated mixed-layer illite-smectite in recent massive sulfide deposits from the sea floor;Alt;Geology,1991

2. Mineralogy and geochemistry of active and inactive chimneys and massive sulfide, Middle Valley, northern Juan de Fuca Ridge: An evolving hydrothermal system;Ames;Can. Mineral.,1993

3. Distribution of selenium in high-temperature hydrothermal sulfide deposits at 13° North, East Pacific Rise;Auclair;Can. Mineral.,1987

4. Some ore textures involving sphalerite from the Furutobe Mine, Akita Prefecture, Japan;Barton;Min. Geol.,1978

5. Chalcopyrite disease in sphalerite: Pathology and epidemiology;Barton;Am. Mineral.,1987

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