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2016
A. A. Sappin, Houlé, M. G., Lesher, C. M., McNicoll, V., Vaillancourt, C., and Kamber, B. S., Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada, Precambrian ResearchPrecambrian Research, vol. 286, pp. 101-125, 2016.
S. J. Piercey, Gibson, H. L., Tardif, N., and Kamber, B. S., Ambient Redox and Hydrothermal Environment of the Wolverine Volcanogenic Massive Sulfide Deposit, Yukon: Insights from Lithofacies and Lithogeochemistry of Mississippian Host Shales, Economic GeologyEconomic Geology, vol. 111, pp. 1439-1463, 2016.
S. J. Piercey, Gibson, H. L., Tardif, N., and Kamber, B. S., Ambient redox and hydrothermal environment of the Wolverine volcanogenic massive sulfide deposit, Yukon: Insights from lithofacies and lithogeochemistry of Mississippian host shales, Economic GeologyEconomic Geology, vol. 111, pp. 1439-1463, 2016.
Compilation and indexing terms, Copyright 2018 Elsevier Inc.20162602541569Hydrothermal alterationsHydrothermal environmentInverse correlationNegative Ce anomalyOrganic-carbon preservationSulfide mineralizationVolcanogenic massive sulfide depositsVolcanogenic massive sulfides
B. Gourcerol, Kontak, D. J., Thurston, P. C., and Petrus, J. A., Application of LA ICP-MS analysis of sulfides to the deconvolution of elemental paragenesis and associations in hydrothermal gold systems, in Geological Society of America, 2016 annual meeting & exposition, vol. 48, Geological Society of America (GSA), Boulder, CO, United States, 2016.
GeoRef, Copyright 2018, American Geological Institute.2017-013917
O. Mahmoodi, Application of physical properties measurements to lithological prediction and constrained inversion of potential field data, Victoria Property, Sudbury, Canada, Laurentian University, 2016.
J. K. Desmarais and Smith, R. S., Approximate semianalytical solutions for the electromagnetic response of a dipping-sphere interacting with conductive overburden, GeophysicsGeophysics, vol. 81, pp. E265-E277, 2016.
J. K. Desmarais and Smith, R. S., Approximate semianalytical solutions for the electromagnetic response of a dipping-sphere interacting with conductive overburden, Geophysics, vol. 81, pp. E265-E277, 2016.
GeoRef, Copyright 2018, American Geological Institute.2016-076679Reid Mahaffy
J. K. Desmarais and Smith, R. S., Benefits of using multi-component transmitter-receiver systems for determining geometrical parameters of a dipole conductor from single-line anomalies, Exploration GeophysicsExploration Geophysics, vol. 47, pp. 1-12, 2016.
Df7iwTimes Cited:0Cited References Count:16
J. K. Desmarais and Smith, R. S., Benefits of using multi-component transmitter-receiver systems for determining geometrical parameters of a dipole conductor from single-line anomalies, Exploration Geophysics (Melbourne), vol. 47, pp. 1-12, 2016.
GeoRef, Copyright 2018, American Geological Institute.2016-087939synthetic data
R. J. Stern, Ali, K. A., Ren, M., Jarrar, G. H., Romer, R. L., Leybourne, M. I., Whitehouse, M. J., and Ibrahim, K. M., Cadomian (~560 Ma) crust buried beneath the northern Arabian Peninsula: Mineral, chemical, geochronological, and isotopic constraints from NE Jordan xenoliths, Earth and Planetary Science LettersEarth and Planetary Science Letters, vol. 436, pp. 31-42, 2016.
GeoRef, Copyright 2018, American Geological Institute.2016-046578
B. Gourcerol, Characterization of banded iron formations associated with gold mineralization: primary geochemical signatures and exploration implications, Laurentian University, 2016.
A. S. Dalton, Finkelstein, S. A., Barnett, P. J., and Forman, S. L., Constraining the Late Pleistocene history of the Laurentide Ice Sheet by dating the Missinaibi Formation, Hudson Bay Lowlands, Canada, Quaternary Science Reviews, vol. 146, pp. 288-299, 2016.
Compilation and indexing terms, Copyright 2018 Elsevier Inc.20162802591355InterstadialMarine incursionMeta analysispre-LGMWISCONSIN
E. Thomas Slater, The Cortaderas Zone, Pirquitas Mine, NW Argentina: An Example of Miocene Epithermal Ag-Zn-Pb-Sn Mineralization in the Andean Tin Belt, Laurentian University, 2016.
J. K. Desmarais and Smith, R. S., Decomposing the electromagnetic response of magnetic dipoles to determine the geometric parameters of a dipole conductor, Exploration GeophysicsExploration Geophysics, vol. 47, pp. 13-23, 2016.
Df7iwTimes Cited:3Cited References Count:21
J. K. Desmarais and Smith, R. S., Decomposing the electromagnetic response of magnetic dipoles to determine the geometric parameters of a dipole conductor, Exploration Geophysics (Melbourne), vol. 47, pp. 13-23, 2016.
GeoRef, Copyright 2018, American Geological Institute.2016-087940
A. Ielpi, Ventra, D., and Ghinassi, M., Deeply channelled Precambrian rivers; remote sensing and outcrop evidence from the 1.2 Ga Stoer Group of NW Scotland, Precambrian ResearchPrecambrian Research, vol. 281, pp. 291-311, 2016.
GeoRef, Copyright 2018, American Geological Institute.2017-018294northwestern ScotlandStoer GroupStoer Peninsula
B. Gourcerol, Thurston, P. C., Kontak, D. J., Côté-Mantha, O., and Biczok, J., Depositional setting of Algoma-type banded iron formation, Precambrian ResearchPrecambrian Research, vol. 281, pp. 47-79, 2016.
B. Gourcerol, Thurston, P. C., Kontak, D. J., Côté-Mantha, O., and Biczok, J., Depositional setting of algoma-type banded iron formation, Precambrian ResearchPrecambrian Research, vol. 281, pp. 47-79, 2016.
GeoRef, Copyright 2018, American Geological Institute.2017-018282Beardmore-Geraldton gold districtMeadowbank DepositMeliadine DepositRankin Inlet BeltWoodburn Lake Belt
D. W. Leverington and Schindler, M., Detection and mapping of black rock coatings using hyperion images: Sudbury, Ontario, Canada, Remote Sensing, vol. 8, 2016.
Compilation and indexing terms, Copyright 2018 Elsevier Inc.20162302478843Classification resultsHyperionHyperSpectralMaximum likelihood classificationsRemote sensing techniquesRock coatingsSmelterSpectral angle mappers
B. Gourcerol, Kontak, D. J., Thurston, P. C., and Duparc, Q., Do Magnetite Layers In Algoma-Type Banded Iron Formations (BIF) Preserve Their Primary Geochemical Signature? A Case Study of Samples From Three Archean BIF-Hosted Gold Deposits, The Canadian MineralogistThe Canadian Mineralogist, vol. 54, pp. 605-624, 2016.
B. Gourcerol, Kontak, D. J., Thurston, P. C., and Duparc, Q., Do magnetite layers in algoma-type banded iron formations (BIF) preserve their primary geochemical signature? A case study of samples from three Archean BIF-hosted gold deposits, The Canadian MineralogistThe Canadian Mineralogist, vol. 54, pp. 605-624, 2016.
GeoRef, Copyright 2018, American Geological Institute.2017-041494Meadowbank DepositMeliadine DepositMusselwhite Deposit
M. Ghinassi, Ielpi, A., Aldinucci, M., and Fustic, M., Downstream-migrating fluvial point bars in the rock record, Sedimentary Geology, vol. 334, pp. 66-96, 2016.
Compilation and indexing terms, Copyright 2018 Elsevier Inc.20160601910017Architectural elementCross-sectional configurationsDegree of confinementErosion resistantFloodplain depositsMeander bendsPoint barPreservation potential
D. J. Kontak and Samson, I., The East Kemptville Sn-Cu-Zn-Ag-In) deposit, Nova Scotia, Canada; a serendipitous past but promising future, in 42nd Colloquium annual general meeting 2016, vol. 52, Atlantic Geoscience Society, Fredericton, NB, Canada, 2016, pp. 80-81.
GeoRef, Copyright 2018, American Geological Institute.790959-43
T. Naprstek and Smith, R. S., The effect of dielectric permittivity on the fields radiated from a radio-frequency electric dipole in a homogeneous whole space, GeophysicsGeophysics, vol. 81, pp. K1-K8, 2016.
M. Schindler, Lanteigne, S., McDonald, A. M., and Hochella, Jr., M. F., Evidence of Cu- and Ni-bearing surface precipitates and adsorption complexes in remediated soils at the nanoscale; a TEM, micro-Raman, and laser-ablation ICP-MS study of mineral surface coatings, A tribute to Frank Christopher Hawthorne, vol. 54. Mineralogical Association of Canada, Ottawa, ON, Canada, pp. 285-309, 2016.
GeoRef, Copyright 2018, American Geological Institute.2017-006101

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