Martabe - G-Resources

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PTAR MARTABE Deposits are of the " High Sulphidation Epithermal" class Closely associated with hydrothermal fluids from an underlying magma Local Sett¡ng
P¡t 1 r Relatively simple geometry with shallow dipping component and steeper elements r Allows for favourable stripping ratios r Close relationship between lithology, alteration, structure and mineralisation 0.01 to 0,50 0.50 to 1.00 1.00 to 2.50 . dt' r.J d' ;i"v P[ I Cro¡. g.clhn -LitÞþgt 2.5f1to 5.00 >= 5.00 Pit 1 Au Block Model - cross secfron
Page 1 and 2: PTAR MARTABE Martabe Geology Resour
Page 3 and 4: PTAR MARTABE Martabe CoW occurs in
Page 5 and 6: p The Sumatran segment of the Plate
Page 7: PTAR MARTABE Geology-Exploration Te
Page 11 and 12: PTAR MARTABE High Sulphidation Styl
Page 13 and 14: PTAR MARTABE Resources & Reserves M
Page 15 and 16: Geology PTAR MARTABE Developing and
Page 17 and 18: PTAR MARTABE Existing Deposits Defi
Page 19 and 20: Barani PTAR MARTABE 2009 work had t
Page 21 and 22: Barani ¡* Resource update currentl
Page 23 and 24: Ramba Joring Two zones PTAR MARTABE
Page 25 and 26: Uluala Hulu PTAR MARTABE Similar to
Page 27 and 28: P¡t 1 PTAR MARTABE Example of abil
Page 29 and 30: PTAR MARTABE Targets range from ext
Page 31 and 32: .'' PTAR MARTABE Kapur-Gambir Distr
Page 33 and 34: PTAR MARTABE Tango Papa Martabe sty

Martabe - G-Resources

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