geophysical, structural and mineralogical signatures of ...k2 k3. 20 | • random ams in breccia •...
TRANSCRIPT
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Geophysical, Structural and Mineralogical Signatures of the Cloncurry Mineral System
CSIRO MINERAL RESOURCES – MULTIPHYSICS TEAM
Jim Austin| 22 May2017
+ Ben Patterson, John Walshe, Renee Birchall, Monica leGras, Richard Lilly, Phil Schmidt, Clive Foss, Dean Hillan and Dave Clark
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Petrophysics Overview
MagSus vs Density
• High density, high MagSus, are dominated by coarse MD magnetite, e.g., Osborne, SWAN.
• High density, medium MagSus(e.g., Cormorant, Maronan) may contain magnetite and pyrrhotite.
• High density negligible MagSuscontain hex. pyrrhotite, sphalerite, galena, pyrite and hematite,
2 |
We start with 1 inch cores
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Petrophysics Overview
MagSus vs Remanence
3 |
• High MagSus, and low Q ratios are dominated by coarse MD magnetite, e.g., Osborne.
• Low MagSus, and high Q are rich in monoclinic pyrrhotite, e.g., Cormorant, Canteen.
• Deposits with low MagSus, and low Q may contain hexagonal pyrrhotite, pyrite or hematite.
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AMS (Anisotropy of Magnetic Susceptibility)
Uncover Cloncurry AMS
• Measureable petrophysical property of rock
• Preferred orientation of crystallographic axes of anisotropic magnetic minerals,
– i.e., the magnetic fabric.
can be used to:• Define strain distribution prior to mineralisation
• K3 is generally the shortening direction
• K1/K2 are perpendicular to shortening, define foliation
4 |
Isotropic (random)
Anisotropic
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Uncover Cloncurry AMS
µCT image of Artemis (ART16C)K1
AMS (Anisotropy of Magnetic Susceptibility)
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AMS can provide information about:
• Strain Fabrics• Shearing• Veining (Dilation)• Sedimentary Banding• Magma Flow• Magmatic Settling• So you need to know about the mineralogy and
the texture to use it effectively
Presentation title | Presenter name6 |
N
90
180
270
Geographiccoordinatesystem
Equal-areaprojection
N=12
K1K2K3
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Correlating Structure with Fabric & Mineralogy
• The best way is to image the mineralogy of the same sample you’ve measured
Presentation title | Presenter name7 |
TIMA (Tescan Integrated Mineral Analyser )
Cloncurry -> 750 samples from ~15 deposits
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8 |
Maronan Pb-Zn Artemis Cu-Zn Canteen Cu-Au Mt Colin Au-Cu
Osborne Cu-Au Starra Cu-Au Monakoff Cu-Au E1 Cu-Au
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9 |
Monakoff Cu-Au E1 Cu-Au
Osborne Cu-Au Ernest Henry Cu-Au SWAN Cu-Au
Canteen Cu-Au Starra Cu-Au
Ernest Henry Cu-Au
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IOCG & ISCG alteration systems
• hydrothermal mineralization:• Highly variable• 50 Ma Post-peak metamorphism• Synchronous with felsic
magmatism• Structurally controlled• Formed during transition from
convergence to transpression then extension
• Mineralization was associated with a number of different alteration types:
1. Pyrrhotite-Calcite Alteration
2. Pyrrhotite-Albite Alteration
3. magnetite-apatite
4. sodic (±calcic) alteration
5. Potassic Alteration
6. Quartz-Chlorite-Hematite alteration (retrograde)
10 |
Reduced
Oxidised
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Redox and Geophysics
11 |
Associated with Cu.
Associated with Pb & Zn
Associated with Apatite Associated with Pyrite
Gawler IOCGs
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Redox & Geophysics
12 |
Associated with Cu.
Associated with Pb & Zn
Associated with Apatite Associated with Pyrite
Cloncurry IOCGs
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Redox Control on Cu• Elevated Cu occurs either side of
an apparent redox boundary
• transition from magnetite into magnetite-pyrrhotite
• U-rich alteration sits on more oxidized side
13 |
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Presentation title | Presenter name14 |
Uranium, assoc with Mt-dominant Sodic Alteration
REDOX BOU
NDARY
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Ternary KTU radiometrics
Presentation title | Presenter name15 |
Industry Geos know about this, they just keep it to themselves
- Mat Brown
How can we learn to recognise this better in drill core???
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Case Study1. Ernest Henry Cu-Au
(Iron-Oxide Cu-Au deposit)
Presentation title | Presenter name16 |
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Sodic Alteration (albite-actinolite magnetite)
• albite-dominated lithologies
• variable amounts of coarse multi-domain magnetite as the phase.
• Associated with moderate to high susceptibilities
17 |
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AMS - Hanging wall (Sodic Alteration)
Uncover Cloncurry AMS
N
90
180
270
Geographiccoordinatesystem
Equal-areaprojection
N=22
K1K2K3
18 |
• SE- dipping shear zone• South plunging lineation• Indicating South over
north movement
• Shear Fabric is Consistent with the thrust ± jog model (e.g., Valenta, 2000)
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Potassic Alteration
• Replacement feldspars (e.g., Albite) by K- Feldspar
• Formation of Iron Sulphidesreduces Susceptibility
19 |
• K-feldspar alteration is often thought to be associated with hematite (based on the reddish color of the K-feldspar).
• However, magnetite is the dominant magnetic phase.
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AMS – Breccia Zone (Potassic Alteration)
Uncover Cloncurry AMS
N
90
180
270
Geographiccoordinatesystem
Equal-areaprojection
N=13
K1K2K3
20 |
• Random AMS in breccia
• No fabric (Isotropic)
• It has destroyed the structural fabrics present
• Potassic alteration (Breccia) overprinted the sodic-calcic alteration
• Structurally and
• Metasomatically.
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Quartz-calcite-chlorite-hematite alteration• Late quartz-calcite-chlorite-pyrite-hematite
alteration is present in a number of deposits • associated with copper and/ or molybdenum
at Ernest Henry, Canteen, Kalman and Merlin • most oxidized style observed in the
Cloncurry district, • as indicated by the presence of pyrite and hematite,
• rather than pyrrhotite and magnetite
• mineralized samples (with such alteration) sit below the Mt- trend on the density/sus plot.
• iron in magnetite is being converted to;• ferromagnesian minerals (e.g., chamosite), • chalcopyrite, pyrite and/or hematite during the
late alteration history.
21 |
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AMS – Quartz-Clacite-Chlorite-Hematite
Uncover Cloncurry AMS22 |
• Horizontal lineation
• Consistent with N-S strike-slip movement in a N-S upright fault.
N
90
180
270
Geographiccoordinatesystem
Equal-areaprojection
N=5
K1K2K3
1.000 1.424 F1.000
1.424L
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Geophysical evidence
Uncover Cloncurry AMS23 |
Magnetics 1st Vertical derivative of RTP
• Vertical derivative of RTP
• This shows 3 parallel magnetic zones coincident with NE-oriented shearzones.
• Bounded on each side by north to NNW oriented faults
• Mineralisation is coincident with the intersection of the N-fault and the NE-fabric
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Inverse Bullseye
• Mineralisation increases on alteration gradient, from Sodic to potassic to hydrolytic alteration
• Mineralisation increases as rocks become more weakly magnetic
• Mineralisation related to oxidation here
24 |
Alteration typeChalcopyrite Chamosite Pyrite Albite Microcline Quartz
And-Alb+Potassic+Calcic 0.00 0.82 0.27 7.41 23.54 10.56Magnetite-Apatite* 3.80 1.84 1.09 1.09 1.09 1.09Potassic (Bt) 0.00 0.29 0.07 58.79 2.80 8.48Potassic (Kf) 0.25 2.27 3.38 2.52 45.91 8.22Potassic+ Cal-Qtz-Py 2.00 1.19 4.03 0.96 31.62 15.88Qtz-Cal-Chl-Py±Cpp±Hem 2.88 10.26 13.96 0.16 2.70 33.56Sodic (Ab-Mt-Ti) 0.00 0.31 0.31 54.96 3.73 2.38Sodic + Potassic (Bt) 0.05 1.12 0.27 20.11 20.00 10.03
Sheet1
DensityCorr K (SI)Q - KoenigsbergerErnest HenryDensity (g/cm3)Mag Sus K (SI)Koenigsberger Ratio (Q)Ernest HenryDensity (g/cm3)Mag Sus K (SI)Q RatioRock TypeErnest HenryDensity (g/cm3)Mag Sus K (SI)Koenigsberger Ratio (Q)
EHM001A2.95307666320.56659137690.8131773982EHM0012.96432494460.61704597750.8125669331EHM0452.77908453960.22098369840.5924725823And-Alb+PotassicAnd-Alb+Potassic+Calcic2.850.190.52
B2.942364360.59132632910.643620933EHM0383.17703290360.37059458980.6341791154And-Alb+Potassic+CalcicMagnetite-Apatite*3.801.841.09
C2.99753381050.69322022630.980902468EHM0392.97004487950.25072607810.882542423And-Alb+Potassic+CalcicPotassic (Bt)2.780.130.36
EHM003A2.70326690040.04758063370.4586489662EHM0032.70553653580.05209250550.4324431252EHM0402.84674472570.27720798250.3814436298And-Alb+Potassic+CalcicPotassic (Kf)3.020.520.83
B2.70175183770.04275200680.4034129607EHM0422.85784391430.18827445770.5268962936And-Alb+Potassic+CalcicPotassic+ Cal-Qtz-Py3.100.410.70
C2.71159086950.06594487610.4352674488EHM0432.72283528380.11573727110.4703482391And-Alb+Potassic+CalcicQtz-Cal-Chl-Py±Cpp±Hem3.270.340.47
EHM004A3.20661735240.48080012885.7626778377EHM0043.01034375230.40906245015.9350053744EHM0442.84882775550.15110787110.4346253615And-Alb+Potassic+CalcicSodic (Ab-Mt-Ti)3.140.760.62
B2.90830847780.35516522284.0795591305EHM0462.66972496460.06633248240.2565881248And-Alb+Potassic+CalcicSodic + Potassic (Bt)2.980.523.31
C2.91610542680.39122199867.9627791551EHM0472.77190366370.08486567140.481729532And-Alb+Potassic+Calcic
EHM005A3.58442308271.71044532081.4178599574EHM0053.79942224911.83866999391.0865427735EHM0053.79942224911.83866999391.0865427735Magnetite-Apatite
B3.78643188431.85213887021.1368668062EHM0032.70553653580.05209250550.4324431252Potassic (Bt)
C4.02741178021.95342579080.7049015568EHM0112.77107898220.11336888650.2570310685Potassic (Bt)
EHM006A3.14720053230.9311563450.4258971343EHM0063.13158689450.81976857410.4512841255EHM0142.86463352830.23051128420.3916991081Potassic (Bt)
B3.19432776240.68281913270.2143809235EHM0253.13124855560.59296792590.7738002904Potassic (Kf)
C3.05323238880.84533024450.7135743187EHM0342.91718283750.29648892480.3059791259Potassic (Kf)
EHM007A2.93632727980.54234032320.9599094179EHM0073.16671845340.62638267580.6507771568EHM0353.03922039180.80304508041.57303366Potassic (Kf)
B3.32187754290.58711555610.6407071509EHM0133.12393639790.81474462690.8458743152Potassic (Kf)
C3.24195053750.7496921480.3517149017EHM0162.82063306180.25888583430.8559473431Potassic (Kf)
EHM008A3.54188153391.1631391240.4010874474EHM0083.53269952781.15193249830.3418897299EHM0173.03770990610.46994991660.7351750644Potassic (Kf)
B3.59730852581.27219904040.2695519978EHM0213.09319154580.42356080710.7311770965Potassic (Kf)
C3.45890852361.02045933060.3550297446EHM0192.95019295170.23658230990.5112208413Potassic+ Cal-Qtz-Py
EHM009A2.96412455260.48685039150.3781326564EHM0092.9334632510.484707690.3978228392EHM0203.27821271210.58633557181.7155712937Potassic+ Cal-Qtz-Py
B2.92565189950.52515140360.3485334486EHM0233.22682491660.69481260750.6514131681Potassic+ Cal-Qtz-Py
C2.9106133010.4421212750.4668024125EHM0283.24320934750.34192863830.2600241763Potassic+ Cal-Qtz-Py
EHM010A3.09888071040.79333377670.840532077EHM0103.09509969930.88015455551.0359498519EHM0302.97849352140.461361730.7827666138Potassic+ Cal-Qtz-Py
B3.09041145260.97828572141.4209688231EHM0312.93432633750.10938054960.2710774522Potassic+ Cal-Qtz-Py
C3.09600693490.86884416820.8463486556EHM0183.29837373680.85330260890.4775495169Qtz-Cal-Chl-Py
EHM011A2.7724524080.13431912560.3278759568EHM0112.77107898220.11336888650.2570310685EHM0263.14450676350.33612356110.5397292543Qtz-Cal-Chl-Py
B2.78818431870.09484827730.1786000202EHM0223.32290254980.03813255070.7875180512Qtz-Cal-Chl-Py-Cpp
C2.75260021980.11093925670.2646172284EHM0333.31454612530.11586581440.0612500395Qtz-Cal-Chl-Py-Hem
EHM013A3.19484494220.92672661610.9343169553EHM0133.12393639790.81474462690.8458743152EHM0012.96432494460.61704597750.8125669331Sodic (Ab-Mt-Ti)
B3.0719173470.74263712750.897629529EHM0063.13158689450.81976857410.4512841255Sodic (Ab-Mt-Ti)
C3.10504690440.7748701370.7056764614EHM0073.16671845340.62638267580.6507771568Sodic (Ab-Mt-Ti)
EHM014A2.85048654290.17956354280.3470936872EHM0142.86463352830.23051128420.3916991081EHM0083.53269952781.15193249830.3418897299Sodic (Ab-Mt-Ti)
B2.85605769140.21395589810.3627135216EHM0092.9334632510.484707690.3978228392Sodic (Ab-Mt-Ti)
C2.88735635060.29801441170.4652901154EHM0103.09509969930.88015455551.0359498519Sodic (Ab-Mt-Ti)
EHM015A3.00413079160.54919705455.6384128369EHM0153.02271136530.49082342867.4102533962EHM0043.01034375230.40906245015.9350053744Sodic + Potassic (Bt)
B3.01441383270.46619606966.9874498389EHM0242.99886464120.3913463130.4637973602Sodic + Potassic (Bt)
C3.04958947150.45707716169.6048975129EHM0362.76339526630.23845409341.1696273875Sodic + Potassic (Kf)
EHM016A2.83762068810.29976756420.7154523746EHM0162.82063306180.25888583430.8559473431EHM0373.12276916691.0500758711.591456882Sodic + Potassic (Kf)
B2.8094751210.23651356471.1021426912EHM0153.02271136530.49082342867.4102533962Sodic+Potassic+Calcic
C2.81480337630.2403763740.7502469633
EHM017A3.12185237720.54932153670.9142901698EHM0173.03770990610.46994991660.7351750644
B3.05382957740.54634240970.7708009034
C2.93744776360.31418580360.5204341202
EHM018A3.34789036621.08620521350.6270052267EHM0183.29837373680.85330260890.4775495169
B3.20259399480.82718227540.503923601
C3.34463684940.64652033780.3017197229
EHM019A3.04724715070.35941779480.6220251078EHM0192.95019295170.23658230990.5112208413
B2.93356168970.17680945570.4664367281
C2.86977001480.17351967920.4452006881
EHM020A3.19928265990.54221244121.0739233895EHM0203.27821271210.58633557181.7155712937
B3.19509467940.50560250521.2247742453
C3.44026079690.71119176892.8480162463
EHM021A3.13766962380.40171033750.6802009995EHM0213.09319154580.42356080710.7311770965
B3.05703686140.43297794980.7705882566
C3.08486815230.4359941340.7427420333
EHM022A3.24049289140.09677161090.5138406639EHM0223.32290254980.03813255070.7875180512
B3.43734244850.01096070350.2343666183
C3.29087230960.00666533771.6143468714
EHM023A3.26315029520.75290607470.7144663756EHM0233.22682491660.69481260750.6514131681
B3.1189869350.5579235140.9202839765
C3.29833751950.77360823370.3194891522
EHM024A2.91146636410.30020808530.3441130472EHM0242.99886464120.3913463130.4637973602
B2.97871896380.41146084390.5931743203
C3.10640859560.46237000980.4541047131
EHM025A3.11697470580.62931617310.8752072973EHM0253.13124855560.59296792590.7738002904
B3.05309646730.46329689170.6983974494
C3.22367449350.68629071280.7477961245
EHM026A3.1419404840.31970858390.5500292852EHM0263.14450676350.33612356110.5397292543
B3.1475814030.32764777770.5430871642
C3.14399840330.36101432150.5260713136
EHM028A3.26368904790.36166378050.2755642345EHM0283.24320934750.34192863830.2600241763
B3.23257293670.33784633310.2609921464
C3.23336605780.32627580120.243516148
EHM030A3.02941133040.47945018130.3830297059EHM0302.97849352140.461361730.7827666138
B2.92944408060.4291333141.2315274135
C2.97662515330.47550169470.7337427221
EHM031A2.98549862860.11124400480.3496708653EHM0312.93432633750.10938054960.2710774522
B2.88981124920.10206299780.2543208492
C2.92766913480.11483464610.209240642
EHM033A3.47668747430.15085203450.057182109EHM0333.31454612530.11586581440.0612500395
B3.21731169930.11037945710.0364942412
C3.24963920230.08636595170.0900737684
EHM034A3.01688397640.29383641950.3332583246EHM0342.91718283750.29648892480.3059791259
B2.79455512140.26132263050.2679786746
C2.94010941460.33430772450.3167003783
EHM035A3.14578791071.022926311.6280007339EHM0353.03922039180.80304508041.57303366
B3.09227188030.83526537361.2780909463
C2.87960138440.55094355761.8130092997
EHM036A2.72257486120.17297824530.9197915651EHM0362.76339526630.23845409341.1696273875
B2.78594295090.27346069031.6069110114
C2.78166798690.26892334470.982179586
EHM037A3.14780750131.12430529691.8245379177EHM0373.12276916691.0500758711.591456882
B3.23028085171.23905804981.6233348566
C2.99021914780.78686426631.3264978718
EHM038A3.10601410730.3379648590.5249543644EHM0383.17703290360.37059458980.6341791154
B3.35550214870.43117539620.8434208227
C3.06958245470.34264351420.5341621591
EHM039A3.05851850430.29162692930.904780895EHM0392.97004487950.25072607810.882542423
B2.9230364780.24449216390.8648026788
C2.92857965610.2160591410.8780436952
EHM040A2.82265698840.26867672420.3992612025EHM0402.84674472570.27720798250.3814436298
B2.84598919580.27908275580.3721138904
C2.87158799270.28386446760.3729557966
EHM042A2.82270825970.12848676280.5043372094EHM0422.85784391430.18827445770.5268962936
B2.84089716220.20057734390.6177463923
C2.90992632110.23575926630.4586052793
EHM043A2.77087679190.17071392370.692967913EHM0432.72283528380.11573727110.4703482391
B2.75707717720.14382570020.4838523332
C2.64055188240.03267218930.2342244712
EHM044A2.86931057220.18257566560.4788950628EHM0442.84882775550.15110787110.4346253615
B2.83617355650.10071755810.4153234743
C2.84099913790.17003038970.4096575473
EHM045A2.72308180050.07284569520.3638882105EHM0452.77908453960.22098369840.5924725823
B2.83727915820.31479940280.7042541762
C2.776892660.27530599740.7092753603
EHM046A2.64166946070.06945017990.3196739013EHM0462.66972496460.06633248240.2565881248
B2.70499400380.06162588110.2157952947
C2.66251142930.06792138620.2342951783
EHM047A2.73904304890.07258169530.4739460388EHM0472.77190366370.08486567140.481729532
B2.76825759140.078990350.4757692989
C2.80841035080.10302496890.4954732585
Mag Sus K (SI)
[CELLRANGE][CELLRANGE]
[CELLRANGE][CELLRANGE][CELLRANGE][CELLRANGE][CELLRANGE][CELLRANGE]
2.84933807002124963.79942224906841242.78041634876317013.02330324234799893.10187663112307853.27008229383718073.13731546175350442.98361683839484560.191758900277952621.83866999393260770.131990892096156470.522806159417737890.405066901159674140.335856133768762110.763331995190970170.51595243120105461And-Alb+Potassic+CalcicMagnetite-Apatite*Potassic (Bt)Potassic (Kf)Potassic+ Cal-Qtz-PyQtz-Cal-Chl-Py±Cpp±HemSodic (Ab-Mt-Ti)Sodic + Potassic (Bt)Density (g/cm3)
Magnetic Susceptibility (SI)
Sheet2
Ernest HenryDensity (g/cm3)Mag Sus K (SI)Koenigsberger Ratio (Q)
And-Alb+Potassic+Calcic2.849338070.19175890030.517869478
Magnetite-Apatite*3.79942224911.83866999391.0865427735
Potassic (Bt)2.78041634880.13199089210.3603911006
Potassic (Kf)3.02330324230.52280615940.8315695565
Potassic+ Cal-Qtz-Py3.10187663110.40506690120.6986789242
Qtz-Cal-Chl-Py±Cpp±Hem3.27008229380.33585613380.4665117155
Sodic (Ab-Mt-Ti)3.13731546180.76333199520.6150484394
Sodic + Potassic (Bt)2.98361683840.51595243123.3140280801
assay vs mag
Ernest HenryDensity (g/cm3)Mag Sus K (SI)Q RatioRock TypePrimary phasesChalcopyriteChamositePyriteAlbiteMicroclineQuartzAlteration typeChalcopyriteChamositePyriteAlbiteMicroclineQuartz
EHM0452.77908453960.22098369840.5924725823And-Alb+PotassicEHM0450.010.290.5121.04419.35And-Alb+Potassic+Calcic0.000.820.277.4123.5410.56
EHM0383.17703290360.37059458980.6341791154And-Alb+Potassic+CalcicEHM03801.330.027.3731.5219.35Magnetite-Apatite*3.801.841.091.091.091.09
EHM0392.97004487950.25072607810.882542423And-Alb+Potassic+CalcicEHM03901.030.080.1923.2522.02Potassic (Bt)0.000.290.0758.792.808.48
EHM0402.84674472570.27720798250.3814436298And-Alb+Potassic+CalcicEHM04002.910.037.4225.817.62Potassic (Kf)0.252.273.382.5245.918.22
EHM0422.85784391430.18827445770.5268962936And-Alb+Potassic+CalcicEHM0420.010.930.490.9727.557.41Potassic+ Cal-Qtz-Py2.001.194.030.9631.6215.88
EHM0432.72283528380.11573727110.4703482391And-Alb+Potassic+CalcicEHM04300.280.011.9812.839.18Qtz-Cal-Chl-Py±Cpp±Hem2.8810.2613.960.162.7033.56
EHM0442.84882775550.15110787110.4346253615And-Alb+Potassic+CalcicEHM04400.150.432.2619.875.63Sodic (Ab-Mt-Ti)0.000.310.3154.963.732.38
EHM0462.66972496460.06633248240.2565881248And-Alb+Potassic+CalcicEHM04600.24023.6728.894.47Sodic + Potassic (Bt)0.051.120.2720.1120.0010.03
EHM0472.77190366370.08486567140.481729532And-Alb+Potassic+CalcicEHM04700.210.871.791.170.05
EHM0053.79942224911.83866999391.0865427735Magnetite-ApatiteEHM00500.39017.660.050.23
EHM0032.70553653580.05209250550.4324431252Potassic (Bt)EHM00300.10.0164.640.120.86
EHM0112.77107898220.11336888650.2570310685Potassic (Bt)EHM01100.360.1370.580.70.12
EHM0142.86463352830.23051128420.3916991081Potassic (Bt)EHM0140.010.410.0641.157.594.45
EHM0133.12393639790.81474462690.8458743152Potassic (Kf)EHM01300.80.682.5920.713
EHM0162.82063306180.25888583430.8559473431Potassic (Kf)EHM0160.076.510.796.0849.077.86
EHM0173.03770990610.46994991660.7351750644Potassic (Kf)EHM0170.092.534.454.3629.98.77
EHM0213.09319154580.42356080710.7311770965Potassic (Kf)EHM0210.231.82.651.3342.988.29
EHM0253.13124855560.59296792590.7738002904Potassic (Kf)EHM0250.950.797.550.0152.714.34
EHM0342.91718283750.29648892480.3059791259Potassic (Kf)EHM0340.330.465.28066.476.77
EHM0353.03922039180.80304508041.57303366Potassic (Kf)EHM0350.0932.243.2459.578.53
EHM0192.95019295170.23658230990.5112208413Potassic+ Cal-Qtz-PyEHM0191.242.681.585.4711.3227.87
EHM0203.27821271210.58633557181.7155712937Potassic+ Cal-Qtz-PyEHM0201.450.2311.490.0114.0122.46
EHM0233.22682491660.69481260750.6514131681Potassic+ Cal-Qtz-PyEHM0235.350.564.670.1323.4213.77
EHM0283.24320934750.34192863830.2600241763Potassic+ Cal-Qtz-PyEHM0281.651.932.28027.8820.99
EHM0302.97849352140.461361730.7827666138Potassic+ Cal-Qtz-PyEHM0300.50.392.780.1661.786.92
EHM0312.93432633750.10938054960.2710774522Potassic+ Cal-Qtz-PyEHM0311.81.331.35051.333.28
EHM0183.29837373680.85330260890.4775495169Qtz-Cal-Chl-PyEHM0180.1613.3422.720.652.8735.41
EHM0263.14450676350.33612356110.5397292543Qtz-Cal-Chl-PyEHM0263.190.533.7605.8348.11
EHM0223.32290254980.03813255070.7875180512Qtz-Cal-Chl-Py-CppEHM0223.2625.428.1102.0920.97
EHM0333.31454612530.11586581440.0612500395Qtz-Cal-Chl-Py-HemEHM0334.91.751.2400.0129.73
EHM0012.96432494460.61704597750.8125669331Sodic (Ab-Mt-Ti)EHM00100.140.3278.090.10.08
EHM0063.13158689450.81976857410.4512841255Sodic (Ab-Mt-Ti)EHM00600.48041.2916.492.3
EHM0073.16671845340.62638267580.6507771568Sodic (Ab-Mt-Ti)EHM00700.281.5370.460.923.44
EHM0083.53269952781.15193249830.3418897299Sodic (Ab-Mt-Ti)EHM00800.34020.150.275.54
EHM0092.9334632510.484707690.3978228392Sodic (Ab-Mt-Ti)EHM0090.010.27059.354.562.89
EHM0103.09509969930.88015455551.0359498519Sodic (Ab-Mt-Ti)EHM01000.370.0260.390.040.02
EHM0043.01034375230.40906245015.9350053744Sodic + Potassic (Bt)EHM00400.21039.833.60.38
EHM0242.99886464120.3913463130.4637973602Sodic + Potassic (Bt)EHM0240.110.350.9512.312.8620.39
EHM0362.76339526630.23845409341.1696273875Sodic + Potassic (Kf)EHM0360.061.610.0125.9640.3611.86
EHM0373.12276916691.0500758711.591456882Sodic + Potassic (Kf)EHM0370.041.690.347.1843.247.45
EHM0153.02271136530.49082342867.4102533962Sodic+Potassic+CalcicEHM0150.031.760.0715.279.9310.07
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Thrust-Jog Model
Uncover Cloncurry AMS25 |
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Structural-Geophysical-Geochemical Model
Uncover Cloncurry AMS26 |
Marshall shear is cut by breccia/ orepipe where intersected by the drillhole
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What else can we do??
Presentation title | Presenter name27 |
1. Mineralogy2. Geochemistry3. Hyperspectral4. Conductivity5. Density6. Mag Sus7. Remanence8. Radiometrics
Standard 1 inch paleomag cylinder
After use samples can be also used for
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What WILL we do??
Presentation title | Presenter name28 |
1. Mineralogy2. Geochemistry3. Hyperspectral4. Conductivity5. Density6. Mag Sus7. Remanence8. Radiometrics
Standard 1 inch paleomag cylinder
After use samples can be also used for
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Exploration significance
• Understanding Zonation can help us discriminate barren vs mineralised geophysical anomalies
• Understanding Redox can help us use geophysics to better map mineral systems
• Understanding the relationships between different geophysical signatures of alteration assemblages can help us target them indirectly
• All of this can help us recognise “near miss” signatures in core
Presentation title | Presenter name29 |
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“In theory there is no difference between theory and practice.
In practice there is.”Yogi Berra
the Facts and the Truth30 |
Geophysical, Structural and Mineralogical Signatures of the Cloncurry Mineral System Petrophysics OverviewPetrophysics OverviewAMS (Anisotropy of Magnetic Susceptibility)AMS (Anisotropy of Magnetic Susceptibility)AMS can provide information about:Correlating Structure with Fabric & MineralogySlide Number 8Slide Number 9IOCG & ISCG alteration systemsRedox and GeophysicsRedox & GeophysicsRedox Control on CuSlide Number 14Ternary KTU radiometricsSlide Number 16Sodic Alteration (albite-actinolite magnetite)�AMS - Hanging wall (Sodic Alteration)Potassic AlterationAMS – Breccia Zone (Potassic Alteration)Quartz-calcite-chlorite-hematite alterationAMS – Quartz-Clacite-Chlorite-HematiteGeophysical evidenceInverse BullseyeThrust-Jog ModelStructural-Geophysical-Geochemical ModelWhat else can we do??What WILL we do??Exploration significanceSlide Number 30