1 edition of giant Kidd Creek volcanogenic massive sulfide deposit found in the catalog.
giant Kidd Creek volcanogenic massive sulfide deposit
|Statement||Mark D. Hannington and C. Tucker Barrie, editors.|
|Series||Economic geology monograph -- 10|
|Contributions||Hannington, Mark D. 1962-, Barrie, C. Tucker 1956-|
|The Physical Object|
|Pagination||672 p. :|
|Number of Pages||672|
|LC Control Number||99-76118|
The volcanogenic massive sulfide deposit Kidd Creek, Canada, has average concentrations of mg g −1 Cu, mg g −1 Zn, mg g −1 Pb, mg g −1 Ag and minor concentrations of Sn and Cd (Bleeker and Parrish, , Schandl and Wicks, ).Cited by: 7. Within the context of a structural–stratigraphic analysis of the giant Kidd Creek Cu–Zn–Ag deposit, precise U–Pb zircon ages have been obtained for five critical rock units associated with the e, flow-banded footwall rhyolite is dated at ± Ma, slightly younger than a previously published age of ± 2 Ma on nearby rhyolite by:
Polished section (PPL) showing crystalline aggregate of arsenopyrite (asp) in massive sphalerite (sp), typical of the main sphalerite lens. Giant Kidd Creek Volcanogenic Massive Sulfide deposit, Western Abitibi Subprovince, Timmins, Ontario, Canada. The Phalabowra (Palabora) carbonatite-hosted magnetite–copper sulfide deposit, South Africa: an end-member of the iron oxide–copper–gold–rare earth element deposit group? Mineralium Deposita 36 Author: John Ridley.
Volcanogenic Massive Sulfide Occurrence Model stockwork of the giant Kidd Creek orebody in Canada is also economically important, as it has been mined for decades (see Hannington and others, ). Examples of modern stock- 6. Physical Description of DepositFile Size: KB. the giant Kidd Creek volcanogenic massive sulfide deposit (copper, zinc, tin, silver). Currently in the fourth year of her doctorate at Laurentian, Michelle focuses her research on the volcanic reconstruction of mafic to intermediate flows and associated volcaniclastic units directly.
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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 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 volcanogenic massive sulfide deposit: Western Abitibi Subprovince, Canada. PDF | On Jan 1,M.D. Hannington and others published The giant Kidd Creek volcanogenic massive sulfide deposit, western Abitibi subprovince, Canada: Preface and introduction |.
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.
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.
(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 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 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.
The Giant Kidd Creek Volcanogenic Massive Sulfide Deposit, Western Abitibi Subprovince, Canada: Summary and Synthesis.M.
Hannington, C. Barrie, and W. Bleeker 4 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. Other format(s) available: PDF.
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 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.
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. 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. The ore deposit is hosted by the Kidd Volcanic Complex which is part of the to Ga Kidd-Munro assemblage, that in turn lies within the western Abitibi-Wawa Sub-province of the Superior Province.
Kidd Creek Cu-Zn-Ag volcanogenic massive sulfide (VMS) deposit, within the Abitibi greenstone belt of the Superior prov-ince (Figs. 1 and 2). The NR has been interpreted as a lateral extension of.
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.
Hypogene Gangue Characteristics. Carbonate minerals tend to be widely distributed, but in some metal contents of the Ruttan volcanogenic massive sulfide deposit, northern Manitoba, Canada: Mineralium Deposita, and Barrie, C.T., eds., The giant Kidd Creek volcano-genic massive sulfide deposit, western Abitibi subprovince, Canada.
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 .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. Kidd Mine and Met Site collectively employ approximately employees and y: Canada.Kidd Creek Massive Sulfide Project (NRCan-GSC Project), Principal Investigator, ; Massive Sulfide Deposits, Central Newfoundland (GSC Project), Principal Investigator, ; Juan de Fuca Ridge Studies (U.S.-Canada), Co-Investigator,