Lecture 14 resources 5 sediment hosted Flashcards
Sediment hosted copper deposits
Where do sediment hosted deposits form
sedimentary rocks
examples of large deposits
Periman basin - europe (UK to germany)
Katangan basin - Zambia
80% of the deposits are in these two basins
Process of Cu redistribution is common, rare for this to cause substantial ore.
Special variations of common basin processes
must have acted to have formed the supergiants.
how much do sediment hosted contribute economically
a quarter (25%) of the worlds copper production.
second most important after porphyry.
- many of the giant and super giant = very high grade (higher than porphyry) = good for production.
explain the red bed concept
Red beds, interact with salty brines
there are different rocks above - basement rocks are the metal source (igneous volcanic rocks) where the copper originates from.
red beds - weathering of the basement rock - interacted with residual brines.
initially oxidising ->reducing conditions which is where mineralisation occurs and copper is precipitated.
What is malachite?
hydrated copper carbonate
What’s a EHPH diagram
Diagram presents how copper as hydrated copper chloride compounds are mobilised in this brines and deposited as different copper Minerals at different conditions.
oxidising conditions
EHPH is an indicator
above 0 = oxidising conditions and mobile
below 0 = reducing conditions and precipitated
What’s the Permian Basin
North sea to UK and Germany
Explain the geology of the Zambian mine
Geology: Granite bedrock, then sandstone and conglomerates, then reducing layer (shale, siltstone)
most mines are located along this reducing layer of shale and siltstone.
Granite is the source of copper - mobilised through leaching by brines and deposited in the overlaying rocks.
tectonics play a role - there is rock deformation in the rocks - there are sulphides
what is the difference between porphyry copper and sediment hosted copper deposits.
porphyry deposits = magmatic and igneous
sediment hosted = leaching from base rock