Gourcerol, Blandine, Kontak, Daniel J., Thurston, Phillips C., Duparc, Quentin (2016) 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 Mineralogist, 54 (3) 605-624 doi:10.3749/canmin.1500090

See Also

These are possibly similar items as determined by title/reference text matching only.

	Gourcerol, Blandine, Kontak, Daniel J., Thurston, Phillips C., Petrus, Joseph A. (2018) Application of La-Icp-Ms Sulfide Analysis and Methodology For Deciphering Elemental Paragenesis and Associations In Addition To Multi-Stage Processes In Metamorphic Gold Settings. The Canadian Mineralogist, 56 (1) 39-64 doi:10.3749/canmin.1700048
	Gourcerol, B., Thurston, P.C., Kontak, D.J., Côté-Mantha, O., Biczok, J. (2016) Depositional setting of Algoma-type banded iron formation. Precambrian Research, 281. 47-79 doi:10.1016/j.precamres.2016.04.019
	Gourcerol, B., Kontak, D. J., Thurston, P. C., Petrus, J. A. (2018) Results of LA-ICP-MS sulfide mapping from Algoma-type BIF gold systems with implications for the nature of mineralizing fluids, metal sources, and deposit models. Mineralium Deposita, 53 (6) 871-894 doi:10.1007/s00126-017-0788-7
	Gatsé Ebotehouna, Chesther, Xie, Yuling, Adomako-Ansah, Kofi, Gourcerol, Blandine, Qu, Yunwei (2021) Depositional Environment and Genesis of the Nabeba Banded Iron Formation (BIF) in the Ivindo Basement Complex, Republic of the Congo: Perspective from Whole-Rock and Magnetite Geochemistry. Minerals, 11 (6) 579 doi:10.3390/min11060579
	Gourcerol, B., Thurston, P.C., Kontak, D.J., Côté-Mantha, O. (2015) Interpretations and implications of LA ICP-MS analysis of chert for the origin of geochemical signatures in banded iron formations (BIFs) from the Meadowbank gold deposit, Western Churchill Province, Nunavut. Chemical Geology, 410. 89-107 doi:10.1016/j.chemgeo.2015.06.008
	Gourcerol, B., Thurston, P.C., Kontak, D.J., Côté-Mantha, O. (2017) Corrigendum to “Interpretations and implications of LA ICP-MS analysis of chert for the origin of geochemical signatures in banded iron formations (BIFs) from the Meadowbank gold deposit, Western Churchill Province, Nunavut”. Chemical Geology, 449. 270 doi:10.1016/j.chemgeo.2015.08.021
	Bowins, R. J., Crocket, J. H. (2011) MONAZITE, XENOTIME AND REE MINERALS IN ARCHEAN BANDED IRON-FORMATION FROM THE SHERMAN AND ADAMS MINES, ONTARIO, CANADA. The Canadian Mineralogist, 49 (3) 749-763 doi:10.3749/canmin.49.3.749
	Taner, Mehmet F., Chemam, Madjid (2015) Algoma-type banded iron formation (BIF), Abitibi Greenstone belt, Quebec, Canada. Ore Geology Reviews, 70. 31-46 doi:10.1016/j.oregeorev.2015.03.016
	Moon, Inkyeong, Lee, Insung, Yang, Xiaoyong (2017) Geochemical constraints on the genesis of the Algoma-type banded iron formation (BIF) in Yishui County, western Shandong Province, North China Craton. Ore Geology Reviews, 89. 931-945 doi:10.1016/j.oregeorev.2017.08.005
	Thurston, P. C., Kontak, D. J., & Côté-Mantha, O. (2014). Interpretations and Implications of Preliminary LA ICP-MS Analysis of Chert for the Origin of Geochemical Signatures in Banded Iron-formations (BIFs) from the Meadowbank Gold Deposit, Western Churchill Province, Nunavut. Geological Survey of Canada.
	Petrophysical Characteristics of BIF Hosted Gold Deposits and the Application of Downhole EM to their Exploration, with Examples from Hill 50 Gold Mine, Mt Magnet, Western Australia