Lecture 15 resources 6 VMS Flashcards

Volcanogenic massive sulphide deposits

1
Q

What plate tectonics are we thinking about for VMS deposits

A

constructive plate margins (sea floor spreading) which forms new ocean floor (presence of

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2
Q

what is the relationship between destructive plate margins and copper

A

there are more porphyry copper deposits at destructive plate margins.

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3
Q

What the hydrothermal process

A

heat of the crystalising magma generates a system where cold seawater is drawn in - warms, interacts with the rocks and becomes boyaunt - back to the surface - discharges as a focussed discharge of hydrothermal, fluid and precipitating sulphate.

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4
Q

where is the Cayman trough

A

between Cuba and mexico - part of the Caribbean

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5
Q

Cayman trough

A

one of the deepest areas on the ocean floor.
- vent sites and chimney structures - hot hydrothermal fluid vented onto the sea floor which changes solubility of the fluid - rapid precipitation occurs.
cayman trough has increases of gold.

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6
Q

what’s the content within the chimneys (VMS) how does this compare to porphyry

A

very enriched copper and zinc.
- 1-10% zinc
- 1-10% copper
much higher than porphyry which was at 0.7% copper.

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7
Q

What are the location of major ODP/IODP drilling campaigns on massive sulfides

A

International ocean drilling programme
Ship that drills on the sea floor, actively investigates the ocean floor
Leg 158 TAG
Leg 169 middle valley
Leg 193 pacmanus
Leg 376 Brothers

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8
Q

Trans-Atlantic geothermal (TAG) sulphide deposit

A

formation of TAG -
Precipitated sulphide, beneath that there is anhydrate pyrite stock work zone of alteration - as the fluids are drawn up they alter the host rock, discharged as a black smoke complex.

simple model to underpin all: Magma chamber source which is generating new crust (constructive plate margin) , hydrothermal system = influx of sea water. the reaction and heating up of rocks above sea water, returning to sea floor, black smoke and precipitation of massive sulphides.

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9
Q

is TAG different from Cayman trough and bent hill

A

Both have sulphide mound, drawing in sea water, reacting and returning to surface, black smoke.

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10
Q

what things precipitate at sulphite mounds for VMS?

A

Iron, copper, lead and zinc sulphide precipitate

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11
Q

how is pacmanas different

A

another vent field
- they drilled through hydrothermal vents to understand systems better.

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12
Q

what are complications with drilling?

A
  • don’t want it to get stuck - prevelant at hydrothermal sites because of all the rubble.
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13
Q

What deposits are found in VMS

A

Copper, zinc, lead in the ancient geological record

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14
Q

are VMS geographically restricted

A

no, they occur everywhere but near plate margins - they need to come from the ocean into land via tectonic processes, they represent zones of previous seafloor activity - ancient mid-ocean ridges - now abducted onto land.

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15
Q

Rio tinto mine copper mine, spain

A

Active 1873 -2001
reopened in 2020 for gold
viability of a mineral deposit - depends on multiple deposit types.
- because we can mine lower grade copper - can revisit less strongly mineralised sites.

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16
Q

What are the three ways to make copper deposit

A

1) Arc environment - volcano and subduction zone, melting of the lower mantle generates magma - hydrothermal fluid takes copper into vein systems at higher concentrations

2) sedimentary basins - oxidised red beds, stripping copper from rock - separating at redox.

3) ocean ridges - volcanic massive sulphide, generated of constructive plate margins - heats up builds sulphide mound, takes copper from sig volume of rock and reprecipitates in smaller denser volume.