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magmatic sulfiderich nickelcopper deposits related to

Magmatic sulfide-rich nickel-copper deposits related to

Magmatic sulfide deposits containing nickel (Ni) and copper (Cu), with or without (?) platinum-group elements (PGEs), account for approximately 60 percent of the world's Ni production and are active exploration targets in the United States and elsewhere.

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(PDF) Magmatic Sulfide-Rich Nickel-Copper Deposits

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes: A Preliminary Deposit Model

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Magmatic Sulfide-Rich Nickel-Copper Deposits Related to

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes: A Preliminary Deposit Model . By Klaus J. Schulz, Val W. Chandler, Suzanne W. Nicholson, Nadine Piatak, Robert R. Seal, II, Laurel G. Woodruff, and Michael L. Zientek . Open-File Report 2010–1179 . U.S. Department of the Interior

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USGS Open-File Report 2010-1179: Magmatic Sulfide-Rich

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes: A Preliminary Deposit Model By Klaus J. Schulz 1, Val W. Chandler 2, Suzanne W. Nicholson 1, Nadine Piatak 1, Robert R. Seal, II 1, Laurel G. Woodruff 3, and Michael L. Zientek 4

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Magmatic sulfide-rich nickel-copper deposits related to

The item Magmatic sulfide-rich nickel-copper deposits related to picrite and (or) tholeiitic basalt dike-sill complexes : a preliminary deposit model, by Klaus J. Schulz [and others], (electronic resource) represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in Public Libraries of Suffolk County, New York.

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Occurrence model for magmatic sulfide-rich nickel-copper

Magmatic Ni-Cu±PGE sulfide deposits are spatially and genetically related to bodies of mafic and/or ultramafic rocks. The sulfide deposits form when the mantle-derived mafic and/or ultramafic magmas become sulfide-saturated and segregate immiscible sulfide liquid, commonly following interaction with continental crustal rocks.

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Magmatic Sulfide-Rich Nickel-Copper Deposits Related to

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes

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(PDF) Magmatic Sulfide-Rich Nickel-Copper Deposits

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes: A Preliminary Deposit Model

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Magmatic sulfide-rich nickel-copper deposits related to

Magmatic sulfide rich nickel copper deposits related to picrite and (or) tholeiitic basalt dike sill complexes Uniform series Open-file report (Geological Survey (U.S.)) ; 2010-1179. Notes Title from PDF title screen (USGS, viewed Oct. 26, 2010). Includes bibliographical references. Subject headings Sulfides--United States. Platinum group.

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Magmatic sulfide-rich nickel-copper deposits related to

Magmatic sulfide rich nickel copper deposits related to picrite and (or) tholeiitic basalt dike sill complexes Related names. Contributor: Schulz, K. J. Geological Survey (U.S.) Subjects. Sulfides — United States. Platinum group. Mines and mineral resources — United States. Basalt. Series. Open-file report (Geological Survey (U.S.)) ; 2010-1179. Summary Contents. Other information. Title

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Magmatic sulfide-rich nickel-copper deposits related to

IUCAT is Indiana University's online library catalog, which provides access to millions of items held by the IU Libraries statewide.

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Magmatic sulfide-rich nickel-copper deposits related to

The item Magmatic sulfide-rich nickel-copper deposits related to picrite and (or) tholeiitic basalt dike-sill complexes : a preliminary deposit model, by Klaus J. Schulz [and others], (electronic resource) represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in Public Libraries of Suffolk County, New York.

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Magmatic Sulfide-Rich Nickel-Copper Deposits Related

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (or) Tholeiitic Basalt Dike-Sill Complexes

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Magmatic Sulfide-Rich Nickel-Copper Deposits Related

Magmatic Sulfide-Rich Nickel-Copper Deposits Related to Picrite and (Or) Tholeiitic Basalt Dike-Sill Complexes-A Preliminary Deposit Model: Open-File Report 2010-1179: Schulz, Klaus J, U S Department of the Interior, United, Et Al: Amazon: Libros

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USGS Scientific Investigations Report 2010–5070–I

Occurrence Model for Magmatic Sulfide-Rich Nickel-Copper-(Platinum-Group Element) Deposits Related to Mafic and Ultramafic Dike-Sill Complexes Chapter I of Mineral Deposit Models for Resource Assessment By Klaus J. Schulz, Laurel G. Woodruff, Suzanne W. Nicholson, Robert R. Seal II, Nadine M. Piatak, Val W. Chandler, and John L. Mars

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MAGMATIC SULFIDE DEPOSITS (MODELS 1, 2b, 5a, 5b, 6a, 6b

Figure 1. A, Schematic section of a magmatic sulfide deposit showing the vertical gradation downward from disseminated to massive ore.B, Generalized map showing massive sulfide mineral concentrations in footwall embayments of the Sudbury Complex (Canada). sequences may be related to major lithologic features such as cyclic-unit boundaries, unconformities, chromite seams,

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Magmatic Ore Deposits in Layered Intrusions—Descriptive

Magmatic ore deposits are derived from accumulations of crystals of metallic oxides, or immiscible sulfide, or oxide liquids that formed during the cooling and crystallization of magma, typically with mafic to ultramafic compositions. “PGE reefs” are stratabound PGE-enriched lode mineralization in mafic to ultramafic layered intrusions. The term “reef” is derived from Australian and

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