The giant Kidd Creek volcanogenic massive sulfide deposit

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The giant Kidd Creek volcanogenic massive sulfide deposit in the western Abitibi subprovince of Canada is the largest known deposit of this age currently in production. The Superior province is the world’s largest exposed Archean craton, occupying an area of more than million km 2, bounded by the Trans-Hudson orogen to the west and the Grenville province to the east.

The Kidd Creek volcanogenic massive sulfide (VMS) deposit, located 25 km north of Timmins, Ontario, was discov-ered in by drill testing a strong, air-borne electromagnetic conductor follow-ing an innovative, geological exploration program implemented by Texas Gulf Sul-phur.

The giant Kidd Creek volcanogenic massive sulfide deposit in the western Abitibi subprovince of Canada is the largest known deposit of this age currently in production.

The Superior province is the world’s largest exposed Archean craton, occupying an area of more than million km2, bounded by the Trans-Hudson orogen to the west and the Grenville province to the east.

The giant Kidd Creek volcanic-associated massive sulfide (VMS) deposit in the western Abitibi Subprovince of Canada is unique in that it is a singular deposit rather than one of many in a district.

The giant Kidd Creek volcanogenic massive sulfide deposit: Western Abitibi Subprovince, Canada. The Giant Kidd Creek Volcanogenic Massive Sulfide Deposit, Western Abitibi Subprovince, Canada: Summary and Synthesis.M. Hannington, C. Barrie, and W. Bleeker 4 Volcanogenic massive sulphide (VMS) deposits, also known as volcanic-associated, volcanic-hosted, and volcanosedimentary-hosted massive sulphide deposits, are major sources of Zn, Cu, Pb, Ag, and Au, and significant sources for Co, Sn, Se, Mn, Cd, In, Bi, Te, Ga, and Ge.

They typically occur as lenses of polymetallic massive sulphide that form at or near the seafloor in submarine volcanic. Hydrothermal Alteration Volcanogenic Massive Sulfide Occurrence Model Scientific Investigations Report ––C U.S.

Department of the Interior giant Kidd Creek deposit, where most mineralization occurred below the seafloor in permeable, fragmental felsic Size: KB.

The Giant Kidd Creek Volcanogenic Massive Sulfide Deposit, Western Abitibi Subprovince, Canada: Economic Geology Monogr p. Yang, K., and Scott, S.D.,Geochemical relationships of felsic mag-mas to ore metals in massive sulfide deposits of the Bathurst mining camp, Iberian Pyrite Belt, Hokuroko district and the Abitibi Belt, in.

The Archean North Rhyolite is a bimodal suite of rocks located directly northwest of, but structurally separate from, the Kidd Creek volcanogenic massive sulfide deposit, which has produced million tonnes of ore grading wt% Cu, wt% Zn, % Pb and g/t by: 1.

The giant Kidd Creek volcanic-associated massive sulfide deposit, Abitibi Subprovince, Ontario January In book: Volcanic-associated massive sulfide deposits: Processes and examples in. The Giant Kidd Creek Volcanogenic Massive Sulfide Deposit, Western Abitibi Subprovince, Canada.

Other format(s) available: PDF. The Kidd Creek deposit, located 25 km north of Tim-mins, Ontario, in the western Abitibi subprovince (Fig. 1) The Giant Kidd Creek Volcanic-Associated Massive Sulfide Deposit, Abitibi. The Newfoundland Appalachians host more than 40 volcanogenic massive sulphide (VMS) deposits, and each contain > tonnes of sulphide-rich material.

The Giant Kidd Creek volcanogenic. Volcanogenic massive sulfide ore deposits, also known as VMS ore deposits, are a type of metal sulfide ore deposit, mainly copper-zinc which are associated with and created by volcanic-associated hydrothermal events in submarine environments.

These deposits are also sometimes called volcanic-hosted massive sulfide deposits. The density generally is kg/m3. They are predominantly stratiform accumulations of sulfide. Schematic cross-sections of the various volcanogenic massive sulphide (VMS) deposit types depicting host rocks, hydrothermal alteration, and mineralization; from Galley et al.

(b), after the. Massive sulfide deposits with associated carbonate alteration assemblages that are easily accessible to acid water are less likely to produce acid drainage.

Nature of ore Massive sulfide deposits, by definition, contain zones or lenses of massive sulfide minerals, many with sulfide mineral contents exceeding 90. (Table 1). This is followed by the Mt Kidd Creek deposit containing Mt of metal.

The largest known Canadian VMS deposit is the Mt Windy Craggy, but it only contains Mt of metals. The 50 Mt Horne deposit contains Mt of Zn+Cu+Pb, along with over t of Au, making it also a world-class gold deposit (Figb). The Big discount all books!!. The Kidd Creek volcanic hosted massive sulphide (VHMS) deposit lies within the Archaean Superior Craton in the Timmins-Porcupine district, and is located 25 km north of Timmins, Ontario, Canada.

Volcanogenic massive sulfide ores formed billion years ago on an ancient seafloor The Kidd deposit is one of the largest volcanogenic massive sulfide ore deposits in the world, and one of the world's largest base metal deposits.

It lies within the Abitibi greenstone belt. Current operation [ edit ]Country: Canada. The Myra Falls (MF) polymetallic volcanogenic massive sulphide (VMS) deposit is located on Vancouver Island within a series of middle to late Devonian Sicker Group volcanogenic rocks ().This deposit best fits a Kuroko-type or bimodal-felsic model [].While parts of the mine average over 4 g of gold per metric ton of ore, the overall proven mineral reserves for gold grade for the entire mining Author: Daniel Marshall, Carol-Anne Nicol, Robert Greene, Rick Sawyer, Armond Stansell, Ross Easterbrook.

Hannington MD, Barrie CT, Bleeker W (b) The giant Kidd Creek volcanogenic massive sulfide deposit Western Abitibi Subprovince Canada: preface and introduction. Econ Geol Mon –30 Google ScholarAuthor: J.

T. Oliveira, C. Quesada, Z. Pereira, J. X. Matos, A. R. Solá, D. Rosa, L. Albardeiro, A. Díez-Mon. Deposit Type: The Kidd deposit is one of the largest volcanogenic massive sulfide ore deposits in the world, and one of the world's largest base metal deposits.

Ore Geology: Kidd Creek is based on a rich, steeply dipping volcanogenic sulphide deposit .