nickel and cobalt mineral potential in new zealand...pounamu ultramafics. darren complex. otago...
TRANSCRIPT
GNS Science
Nickel and Cobalt Mineral Potential in New Zealand
1st May 2018
Patricia Durance, Matthew Hill, Regine Morgenstern, Rose Turnbull, Mark Rattenbury, Rob Smillie, NZP&M
GNS Science
Key Points
The Ni-Co Mineral Systems Model Mineral system Model for Ni-Co New Zealand Geology and Mineralogy
GNS Science Mineral Potential Modelling Approach Data Sources: Data mining and New Analyses GIS-based Modelling Methods – Standard Approach to Mineral Systems
Ni-Co mineral potential in New Zealand Mineral potential maps for Ni-Co Ni-Co data gaps, knowledge gaps, opportunities, research questions
GNS Science
(Dulfer et al., 2016).
Mineral System Model for Ni-Co Mineral Potential in New ZealandMagmatic Ni-Cu-(Co) ± PGE
layered intrusion deposit formation1. Magmatic deposits
Stratiform/Stratabound Ni-Cu basal ultramafic parts of Greenstone Belts
(Komatiitic, Dunitic, Picritic) Gabbroic Intrusion or Synorogenic-synvolcanic
2. Structure-related deposits3. Sedimentary deposits
Laterites (weathering)4. Cu-Au-Co Metasedimentary5. Others
Iron oxide-Cu-Au (IOCG)6. Seafloor Manganese nodules and crusts7. PlacerCo is mined as a by-product of Ni-Cu
Deposit types
GNS Science
New Zealand Geology
1. Magmatic deposits Dunitic Ni-Cu Gabbroic-associated Ni-Cu-(Co)±PGE
2. Structure-related deposits (?)3. Sedimentary deposits
Laterites (weathering)4. Cu-Au-Co Metasedimentary (?)5. Seafloor Manganese nodules and crusts 6. Placer (?)
z
Add Minerals - list
GNS Science
QMAP
Petlab
REGCHEM
MR4510
Geophysical surveys
Regional Soil Geochemistry surveys
*includes new analyses
Data Sources
GNS Science
Some data-mining was undertaken for this project to
improve our geochemical and geological databases in
key locations that were known as high-relevant for the
Li, Ni-Co and REE mineralisation in NZ.
Key NZP&M mineral reports (1,811 new data points)
Scientific papers (479 new data points).
Areas of compilation focused on:
• West Coast (Hohonu Ranges, Paparoa Ranges &
Brunner Ranges); Cobb Valley, NW Nelson; Mandamus,
North Canterbury.
There is still more data that could be compiled.
Data Mining
GNS Science
73 samples analysed at ALS laboratories, Brisbane (90 samples analysed in total; including QAQC)
Multiple techniques used; targeting specific ore and pathfinder elements (different digests; ICP-MS, ICP-AES)
New Targeted Geochemical Analyses
Lithium (23 samples)
Pegmatites (West Coast, Fiordland)
Hydrothermally altered clays/lake sediments (Taupo Volcanic Zone, Coromandel, Auckland, Northland)
REE (24 samples)
Alkaline rocks (Trachytes, granites from West Coast, Fiordland)
Heavy mineral sands (West Coast beaches)
Hydrothermally altered rocks (PaparoaMetamorphic Core Complex; altered rhyolitic clays)
Ni-Co (26 samples)
Ultramafics (Dun Mt, Cobb Igneous Complex, Anita Shear Zone, Hawes Head Ultramafics)
Gabbros and granitoids(NW Nelson, Westland, Fiordland)
Basalts, lamprophyres (Lyttelton volcanics,
Greyschist (Aspiring Lithologic Formation)
GNS Science
The Modelling ProcessExpert scientists Spatial analysis Mineral potential model
Mapping reviews
Matt
GNS Science
GIS Techniques in Mineral Potential Modelling
Rock chip sample buffering
Stream sediment catchment analysis
Geochemical knowledge applied to
geology
Soil surveys
Geophysical data
Mineral information (Petlab)
Fault and structural data
Mineral occurrences
Anomalous
No sample
Non-anomalous
Sampled, butnot analysed
Peraluminous
Weakly-Peraluminous
Sampled, butnot analysed
Metaluminous
-4 -2 0 2 4-3.6 -3.2 -2.8 -2.4 -1.6 -1.2 -0.8 -0.4 0.4 0.8 1.2 1.6 2.4 2.8 3.2 3.6
Z score
1E-05
0.0001
0.001
0.01
0.1
1
10
100
1,000
10,000
100,000
Elem
ent a
ssay
Model scale 100 x 100 m cells
STREAM SEDIMENTS
ROCK CHIP SAMPLES
GEOCHEMICAL STATISTICSSOIL SEDIMENT SAMPLES
DISTANCE ANALYSIS GEOCHEMICAL ROCK CLASSIFICATION
GEOPHYSICAL DATA
GNS Science
Combining the Mappable Component Predictive Maps• Knowledge-driven rather than data driven method
• Data is assigned a Fuzzy membership which is an expert assigned weight of how important the data is (positive or negative) to the predictive map.
• Values also reflect the data quality and importance to the mineral system.
• We have used Fuzzy operators to combine the predictive maps; In particular, we used the Fuzzy gamma function– Effectively an averaging process
– It combined the datasets in the best possible way for this study at the NZ-wide scale.
• Missing data values are tracked through the modelling process.
GNS Science
Mappable components of the Ni-Co mineral system
GNS Science
Fuzzy Logic Spatial Modelling Process
1
2
3
4Ener
gyFl
uid
Enric
hTr
apSu
rfac
e
GNS Science
Mineral Potential Maps for the Magmatic Ni-Co mineral systemResults: High Ni-Co Mineral Potential Areas
Riwaka Igneous Complex
Cobb Igneous Complex
Dun Mountain Ultramafic Group
Patuki Melange
Red Mountain
1 23
Hekeia Gabbro
West Dome4
OtomaIngneousComplex
Nelson and Marlborough
regionsTasman region
South West Coast region
Southland region
GNS Science
Mineral Potential Maps for the Magmatic Ni-Co mineral system
Gaps: The cooler coloured areas are not necessarily fixed. These results can often be attributed to data gaps: Poorly or under-mapped geology and poorly defined boundaries, contacts
and structures Under-sampled / Not sampled Sampled but not analysed
This leads to holes or gaps in knowledge about the mineral system components New Zealand’s magmatic nickel deposits are under-studied The relationship between cobalt and nickel in ultramafic and mafic rocks
is not well understood. Very little is known about cobalt and the other types of deposits it may be
associated with.
Opportunities: Cobalt can and is coupled with other metals, in other globally established
structure-, sedimentary-, and metasedimentary-related deposit types including: copper, PGEs, iron and manganese, and a host of polymetallic vein-types.
For New Zealand, this presents opportunities to explore for cobalt in other settings such as the Otago schist.
Pounamu Ultramafics
Darren Complex
Otago Schist
DMOBPounamu
Ultramafics
GNS Science
Missing data• Data challenges:
– Data exists but is not digital
– Data does not exist
– Data is incorrect or not correctly attributed
• Understanding our missing
data in modelling process.
• Filling in the most important
data gaps to increase our
knowledge of mineral
potential.
Analysed
No sample
Sampled, butnot analysed
Unsampledintrusion
AnalysedSample
Sampled, butnot analysed
SOLUTION: Data compilations
SOLUTION: Sample surveys
SOLUTION: Database design & QA/QC
-4 -2 0 2 4-3.6 -3.2 -2.8 -2.4 -1.6 -1.2 -0.8 -0.4 0.4 0.8 1.2 1.6 2.4 2.8 3.2 3.6
Z score
0.0001
0.001
0.01
0.1
1
10
100
Elem
ent a
ssay PPB
PPM
STREAM SEDIMENTSROCK CHIP SAMPLES
GEOCHEMICAL ROCK CLASSIFICATION
GEOCHEMICAL STATISTICS