Exploration of minerals Flashcards
Concentration factor equation
Grade (%) ÷ average crystal abundance (%)
What is the main ore mineral for copper??
Chalcopyrite CuFes2
what is secondary enrichment??
when metal ore is leeched from within surface rocks and precipitate just below WT
Formation of chalcopyrite
hydrothermal fluids dissolve copper from I rocks
precipitate in surrounding contact met sed rocks
often found in hydrothermal veins
Why don’t we exploit copper from chalcopyrite
Conc factor not high enough
not at cut off grade
part of resource not reserve
inaccessible
Flow diagram for secondary enrichment
(of chalcopyrite)
Chalcopyrite
In forms of sulphides - insoluble in H20
Chalcopyrite exposed and chem weathering /oxidation
produces copper sulphate
this is soluble in H20
percolates down in ground
reaches WT = saturated and anaerobic
reduced + dep as Cu just below WT
now much more conc and econ viable to mine
What is gossan?
an insoluble cap of iron oxide at the surface of a mineral vein
why are gossans useful
marker for Cu below surface left over from secondary enrichment of chalcopyrite
porphyry def
a large igneous intrusion with a porphyritic texture (2 stage cooling)
formation of porphyry cooper dep
flow diagram
form as a result of hydrothermal processes associated with granite intrusions at convergent plate margins
C plate boundary
melting
granite intrusion (S and wet) high H20
M chamber cools and common S minerals form e.g. quartz and feldspar
Leftover= H2O and incompetent metals e.g. Au Cu U Mo called at top of M chamber
some crystals take up more space as solid rather than liquid
less space pressure builds
surrounding C rock fractures
hydrothermal fluid moves away from porphyry and cools
metals are dep /come out of solution along fractures as come out of solution at diff temps
form mineral veins
What is a Placer deposit
surface deposits formed by sed processes of weathering and erosion, transport and dep
why are Placer dep important
Dense physically and chem resistant mineral e.g. cassiterite , gold and diamond can be converted by these processes until small but high grade ore dep
How do Placer deps form?
weathering
ore is broken up by mech/
left as insoluble metals by chem
ore and gangue sep into individual grains
weather metals transported by H20 in river + sea (sorted by grain size hardness and density)
when velocity slows preferentially dep as ore mix with unconsolidated sand and gravel
become conc as resistant to erosion and being dissolved
all mins have sim properties: hard + little cleavage, unreactive so don’t dissolve,dense- dep first
5 places placer deposits form
Meander bends
plunge pools
upstream projections
downstream confluences
on beaches
How do placers form on meandering bends?
current swings around outside bend
velocity higher on outside
lower inside
results in dep on inside (placer dep) and erosion on outside
how do placer deps form in plunge pools
river flows erodes less resistant rock creating waterfall
turbulent water and boulder at bottom of waterfall scour out deep hollow
plunge pool
dense placer min trapped in sed in plunge pool
how do placer deps form at upstream projections
projections e.g. Dykes in river bed will trap dense placer mineral
on upstream side
may be where hard rock projects out or just small scale like ripples
how do placers form downstream of confluences
fast flowing tributary joins slower flow river
current drops
dense placer min dep into mid channel sandbar
how do placers form on beaches
river transport sed to sea
sed move along coast by longshore drift
waves throw sediment up to beach via swash
energy drops in wave during backwash - dense placer minerals deposited
4 geophysical techniques for exploration of minerals
Gravity surveys
magnetic surveys
electromagnetic surveys
electrical resistivity survey
Gravity surveys
gravimeter - measures variations in grav field strengths
shows varied results from rocks and mins
plotted with lines showing equal strengths
+= high density metal ore/ M or UM intrusion
-= low density S intrusion e.g. hydrothermal vein or oil + gas or aquifer
magnetic survey
magnetometer measures variation in mag field strength
+= rich in Mg and Fe
due to M or UM intrusion (may contain cumulate ore dep)
or presence of haematite, magnetite or pyrite
electromagnetic survey
measures ground conductivity using electromagnetic inductor
give value as % of secondary relative field: primary field
electricity produced by transmitted induced current in conductive minerals e.g. metal ore
good for metal sulphide minerals e.g. chalcopyrite
use very low frequency
electrical resistivity survey
2 electrodes placed in ground
pass e current between
if underlying rock good conductor = low res
metals = good conductors so lower res
used for gold exploration