whoi hydrothermal vents videoweb.pdx.edu/~jjackson/30jan17.pdfwhoi hydrothermal vents video. usgs...
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WHOI Hydrothermal Vents Video
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USGS Scientific Investigations 2010-5070-C
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USGS Scientific Investigations 2010-5070-C
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USGS Scientific Investigations 2010-5070-C
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USGS Scientific Investigations 2010-5070-C
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USGS Scientific Investigations 2010-5070-C
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USGS Scientific Investigations 2010-5070-C
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Figure 9-11 Kessler (1994)Mineral Resources, Economics,And the Environment
Some Ore Models
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Water: polar, high dialectric constant, high heat capacity, high surface tension, maximum density above 32°F
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PLUTON
3. Hydrothermal settings- as magmas crystallize, the water present in the liquid magma is driven off into fractures or permeable beds within the host rock. Minerals species that are water-soluble will thus be carried away from the parent magma body. As the water encounters lower temperatures and pressures, it may boil. Sulfide ores will precipitate in the order shown in this diagram, beginning with zinc or lead if present, and ending with a sinter of silica and or carbonate. The host rock may thus become host to hydrothermal deposits. Hydrothermal waters may also be derived from the circulation of ground water in deep basins. If the resulting brines ascend to shallow depths, the same order of precipitation of dissolved sulfides may occur.
Hydrothermal settings Sinter (Silica/Carbonate) Arsenic
Antimony
Mercury
Gold
Silver
Copper
Zinc-Lead
Order of precipitation ofhydrothermal mineralsbetween pluton andsurface
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Figure 3.25 Robb (2005) Introduction To Ore Forming Processes
SEDEX Model
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http://www.pmel.noaa.gov/vents/gallery/R852_DSC_092004_070004_03772.JPG
Sully VentMain Endeaver Vent FieldNE Pacific
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Red Dog Mine: world’s largest zinc producer
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http://m.ammoth.us/blog/wp-content/uploads/2010/03/red-dog-pit-mine_2.jpg
Red Dog Mine Pit
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Kelley et al 2004
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Kelley et al 2004
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Schardt 2016
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Schardt 2016
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Magmatic Processes
• Within the magma chamber• During magmatic ascent• During volcanic venting• The role of water
– Magmatic water– Ground water
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1. Magma Chamber 2. Early Minerals 3. Gravity Settling
Examples: Chromite(FeCr2O4), Ilmenite (FeTiO3) in a mafic magma body. Both are oxides, which crystallize early in a magma’s solidification.
What goes on within the magma chamber?
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Josephine Ophiolite, Klamath Mtns, near Weed, CA
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Harper 1984
Chromite within dunnite
Garick et al 2009
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