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Ok Tedi Deposit

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Journal Article
Journal: Economic Geology
Published: 01 January 2018
Economic Geology (2018) 113 (1): 39–61.
... emplacement and Au-Cu ore formation at Ok Tedi, the Earth’s youngest giant porphyry-skarn deposit. Trace element contents in zircons were obtained by laser ablation-inductively coupled plasma-mass spectrometry before selected grains were removed from the sample mount, chemically abraded, spiked, and dissolved...
FIGURES | View All (16)
Journal Article
Journal: Economic Geology
Published: 01 November 2013
Economic Geology (2013) 108 (7): 1773–1781.
...Michiel Van Dongen; Roberto F. Weinberg; Andrew G. Tomkins Abstract The Ok Tedi porphyry Cu-Au deposit in Papua New Guinea is a world-class mineral deposit. In its pre-mining stage, it contained 5.5 Mt Cu and 18.1 Moz Au; skarn accounts for ~80% of the current 1.9 Mt Cu and 7.7 Moz Au in total...
FIGURES | View All (7)
Journal Article
Journal: Economic Geology
Published: 01 August 2014
Economic Geology (2014) 109 (5): 1493–1494.
... observations at Ok Tedi imply a “very different picture of the relationships between intrusive rocks, host rocks, and mineralization” than the one we proposed. We would argue that his observations are actually broadly consistent with our model, but our interpretation was more concerned with the deposit-scale...
Journal Article
Journal: Economic Geology
Published: 01 August 2014
Economic Geology (2014) 109 (5): 1489–1492.
... and their alteration, Mt Fubilan porphyry copper deposit : Geological Survey of Papua New Guinea, Report 77/5 , 10 p. Arnold G.O. Griffin T. J. Hodge C.C. , 1979 , Geology of the Ok Tedi and southern Atbalmin 1:100000 sheet: Part 3, Igneous rocks and structure : Geological Survey of Papua New...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 December 1972
Economic Geology (1972) 67 (8): 1019–1033.
Image
North-south cross section through the <span class="search-highlight">Ok</span> <span class="search-highlight">Tedi</span> <span class="search-highlight">deposit</span> based on field observ...
Published: 01 January 2018
Fig. 4. North-south cross section through the Ok Tedi deposit based on field observations and drill hole data through the southern part of the pit (A-B in Fig. 3 ). The Fubilan porphyry and the breccias intrude into the monzodiorites and sedimentary rocks. Ore grades indicate enrichment of Cu
Image
Slab photos of rock types at the <span class="search-highlight">Ok</span> <span class="search-highlight">Tedi</span> <span class="search-highlight">deposit</span>. (A, B) Sulfide-rich brecc...
Published: 01 January 2018
Fig. 5. Slab photos of rock types at the Ok Tedi deposit. (A, B) Sulfide-rich breccias range from clast dominated and biotite rich (A) to matrix dominated (B). (C) The Fubilan porphyry contains plagioclase and alkali feldspar phenocrysts generally <1 cm and biotite flakes that form larger
Image
Selected rock relationships observed in the <span class="search-highlight">Ok</span> <span class="search-highlight">Tedi</span> <span class="search-highlight">deposit</span>. (A) Breccia wi...
Published: 01 January 2018
Fig. 8. Selected rock relationships observed in the Ok Tedi deposit. (A) Breccia with a quartz-biotite–cemented sandy matrix crosscutting the biotite monzodiorite. (B) Mafic xenolith cut by a quartz-sulfide vein. (C) Thick quartz-molybdenite-chalcopyrite veins (<1 cm) with a potassic
Image
Simplified regional geology of the <span class="search-highlight">Ok</span> <span class="search-highlight">Tedi</span> <span class="search-highlight">deposit</span> in Papua New Guinea, mod...
Published: 01 November 2013
Fig. 1 Simplified regional geology of the Ok Tedi deposit in Papua New Guinea, modified from Hill et al. (2002) , with schematic north-south cross section (modified from Mason, 1997 ). Intrusions in cross section are in solid black, gray unit is top of Toro sandstone, a marker unit in regional
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Regional geologic map of the Star Mountains in western Papua New Guinea. Th...
Published: 01 January 2018
Fig. 2. Regional geologic map of the Star Mountains in western Papua New Guinea. The Ok Tedi deposit is hosted within the Ok Tedi intrusive complex. The Anju Andesite intrusion is located ~10 km southwest of Ok Tedi. The Ok Tedi anticline and Alice anticline are western splays of the Muller
Image
Geologic map of the <span class="search-highlight">Ok</span> <span class="search-highlight">Tedi</span> porphyry-skarn Au-Cu <span class="search-highlight">deposit</span>. The Sydney and bi...
Published: 01 January 2018
Fig. 3. Geologic map of the Ok Tedi porphyry-skarn Au-Cu deposit. The Sydney and biotite monzodiorite and the later Fubilan porphyry intruded into the surrounding sedimentary sequence. Breccias occur throughout the deposit but the intrusive breccias containing high Au-Cu ore grade
Image
Thin section images in plane-polarized light (A, B) and crossed-polarized l...
Published: 01 January 2018
Fig. 7. Thin section images in plane-polarized light (A, B) and crossed-polarized light (C) of different minerals or replaced minerals within the Ok Tedi deposit. (A) Titanite replaced by ilmenite and other secondary minerals in highly altered Sydney monzodiorite. (B) Secondary biotite and minor
Journal Article
Journal: Economic Geology
Published: 01 August 2013
Economic Geology (2013) 108 (5): 1185–1193.
... the skarn-focused discovery and early production history of the deposit, as well as the presence of several large skarn deposits within the district. The Ok Tedi Cu-Au-Ag deposit of western Papua New Guinea also is generally thought of as a major porphyry Cu deposit, yet hosts both porphyry and skarn...
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Journal Article
Published: 01 August 1978
Journal of the Geological Society (1978) 135 (4): 457.
... affinities are with the deposits in nearby island arcs, then the reason must be found in the existence of some other factor, which might be purely geographical. Furthermore the New Guinea porphyrys, and particularly Ok Tedi, which has been dated at 1·1Ma present difficulties for any theory which proposes...
Journal Article
Published: 01 February 1995
Quarterly Journal of Engineering Geology and Hydrogeology (1995) 28 (1): 47–60.
... engineering feasibility studies began in 1978. Subsequent terrain hazard mapping has identified numerous landslides and rock avalanche deposits in the Ok Tedi catchment and in the immediate vicinity of the mine, ranging from very low frequency, catastrophic rock avalanches through to mudslides and mudflows...
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Geologic map of New Guinea. The four simplified tectonic units are, from so...
Published: 01 January 2018
, and the accreted arcs and terranes. The suggested continuation of the Tasman line into New Guinea (e.g., Baldwinn et al., 2012; Davies, 2012 ) separates Proterozoic basement rocks in the west from Paleozoic basement rocks in the east. The Ok Tedi deposit is located in the southern highlands of the fold-and-thrust
Journal Article
Journal: Economic Geology
Published: 01 June 2010
Economic Geology (2010) 105 (4): 763–776.
... processes, or a combination of both. We investigated whole-rock trace-element and REE patterns of samples from the giant Ok Tedi porphyry copper-gold deposit, Papua New Guinea, and found that REEs were most depleted in zones of greatest hydrothermal alteration. REE-rich accessory phases zircon, apatite...
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Journal Article
Journal: Economic Geology
Published: 01 May 1989
Economic Geology (1989) 84 (3): 506–528.
... saturated porous media and chemical fluid-rock interactions incorporating mineral dissolution kinetics. Field and laboratory analytic and mineralogic data from supergene enrichment systems at Butte, Montana, and Ok Tedi, located in western Papua New Guinea, are used to provide geochemical, lithologic...
Journal Article
Journal: Economic Geology
Published: 01 August 1978
Economic Geology (1978) 73 (5): 796–809.
...H. L. Davies; W. J. S. Howell; R. S. H. Fardon; R. J. Carter; E. D. Bumstead Abstract The Ok Tedi porphyry copper-gold deposit in western Papua New Guinea was discovered and tested by a subsidiary of Kennecott Copper Corporation in 1968-1971. Exploration lapsed in 1972-1975 while Kennecott...
Journal Article
Journal: Economic Geology
Published: 01 August 1975
Economic Geology (1975) 70 (5): 928–936.
... of the Mount Fubilan (Ok Tedi) porphyry copper deposit show a time gap of 1.5 m.y. between initial magmatic emplacement (2.6 m.y.) and subsequent copper mineralization (1.1 m.y.) associated with the Fubilan porphyries. Comparison of the ages of mineralized porphyries in the Star Mountains Intrusives (3.4...