Search Results - "Fedorowich, J. S"

Chlorine and alkali geochemical halos in the footwall breccia and sublayer norite at the margin of the Strathcona Embayment, Sudbury Structure, Ontario by McCormick, K. A, Lesher, C. M, McDonald, A. M, Fedorowich, J. S, James, R. S

“…The Ni-Cu-platinum-group element ores in the sublayer and footwall breccia of the Sudbury structure have distinctive geochemical haloes. In the Fraser mine,…”
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Geodynamic evolution and thermal history of the central Flin Flon Domain, Trans-Hudson Orogen: Constraints from structural development, 40Ar/39Ar, and stable isotope geothermometry by Fedorowich, J. S., Kerrich, R., Stauffer, M. R.

“…Shear zones in the Flin Flon area record five episodes of development. These have been studied using structural analysis and 40Ar/39Ar thermochronology…”
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Variations in Ni content in sheared magmatic sulfide ore at the Thayer Lindsley Mine, Sudbury, Ontario by Bailey, Joshua, McDonald, Andrew M, LaFrance, Bruno, Fedorowich, John S

“…The Thayer Lindsley mine, located in the geographic South Range of the 1.85 Ga Sudbury Igneous Complex (SIC), hosts both contact-style Ni-Cu-PGE sulfide…”
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U-Pb dating of a diabase dike resolves the problem of mutually crosscutting relationships within the Fraser-Strathcona deep copper vein system, Sudbury Basin by Fedorowich, John S, Parris, Randy R, Sager-Kinsman, A

“…The Fraser-Strathcona Deep Copper mine, Sudbury has diabase dykes and a chalcopyrite vein system having a mutually crosscutting relationship. Detailed…”
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Chlorine and Alkali Geochemical Halos in the Footwall Brecciaand Sublayer Norite at the Margin of the Strathcona Embayment, SudburyStructure, Ontario by McCormick, K. A., Lesher, C. M., McDonald, A. M., Fedorowich, J. S., James, R. S.

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A textural, mineralogical, and statistical study of the footwall breccia within the Strathcona Embayment of the Sudbury Structure by McCormick, Kelli A, Fedorowich, John S, McDonald, Andrew M, James, Richard S

“…The footwall breccia is one of the main Ni-Cu-(PGE) ore-hosting units of the Sudbury camp. This polymict, matrix-supported, contact-metamorphosed breccia…”
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Sudbury Breccia (Canada): a product of the 1850 Ma Sudbury Event and host to footwall Cu–Ni–PGE deposits by Rousell, Don H, Fedorowich, John S, Dressler, Burkhard O

“…The Sudbury Structure, formed by meteorite impact at 1850 Ma, consists of three major components: (1) the Sudbury Basin; (2) the Sudbury Igneous Complex, which…”
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Geodynamic evolution and thermal history of the central Flin Flon Domain, Trans-Hudson Orogen: Constraints from structural development, super(40)Ar/ super(39)Ar, and stable isotope geothermometry by Fedorowich, J S, Kerrich, R, Stauffer, M R

“…Shear zones in the Flin Flon area record five episodes of development. These have been studied using structural analysis and super(40)Ar/ super(39)Ar…”
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Geodynamic evolution and thermal history of the central Flin Flon Domain, Trans‐Hudson Orogen: Constraints from structural development, 40 Ar/ 39 Ar, and stable isotope geothermometry by Fedorowich, J. S., Kerrich, R., Stauffer, M. R.

“…Shear zones in the Flin Flon area record five episodes of development. These have been studied using structural analysis and 40 Ar/ 39 Ar thermochronology…”
Get full text

Chlorine and Alkali Geochemical Halos in the Footwall Breccia and Sublayer Norite at the Margin of the Strathcona Embayment, Sudbury Structure, Ontario by McCormick, K. A.

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