Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada
• Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion...
Ausführliche Beschreibung
Gespeichert in:
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Sappin, A.-A. [verfasserIn] |
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Englisch |
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2016 |
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25 |
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Enthalten in: OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study - Salunkhe, R. ELSEVIER, 2017, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:286 ; year:2016 ; pages:101-125 ; extent:25 |
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10.1016/j.precamres.2016.09.018 |
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10.1016/j.precamres.2016.09.018 doi GBVA2016010000004.pica (DE-627)ELV035287284 (ELSEVIER)S0301-9268(16)30383-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 570 540 VZ Sappin, A.-A. verfasserin aut Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada 2016 25 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion younger (2717Ma) and unrelated to Wabassi Intrusive Complex. Miminiska–Fort Hope greenstone belt Elsevier Superior Province Elsevier Layered intrusion Elsevier Ultramafic intrusion Elsevier Mafic intrusion Elsevier Neoarchean Elsevier Houlé, M.G. oth Lesher, C.M. oth McNicoll, V. oth Vaillancourt, C. oth Kamber, B.S. oth Enthalten in Elsevier Science Salunkhe, R. ELSEVIER OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study 2017 Amsterdam [u.a.] (DE-627)ELV014866900 volume:286 year:2016 pages:101-125 extent:25 https://doi.org/10.1016/j.precamres.2016.09.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 AR 286 2016 101-125 25 045F 550 |
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10.1016/j.precamres.2016.09.018 doi GBVA2016010000004.pica (DE-627)ELV035287284 (ELSEVIER)S0301-9268(16)30383-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 570 540 VZ Sappin, A.-A. verfasserin aut Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada 2016 25 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion younger (2717Ma) and unrelated to Wabassi Intrusive Complex. Miminiska–Fort Hope greenstone belt Elsevier Superior Province Elsevier Layered intrusion Elsevier Ultramafic intrusion Elsevier Mafic intrusion Elsevier Neoarchean Elsevier Houlé, M.G. oth Lesher, C.M. oth McNicoll, V. oth Vaillancourt, C. oth Kamber, B.S. oth Enthalten in Elsevier Science Salunkhe, R. ELSEVIER OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study 2017 Amsterdam [u.a.] (DE-627)ELV014866900 volume:286 year:2016 pages:101-125 extent:25 https://doi.org/10.1016/j.precamres.2016.09.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 AR 286 2016 101-125 25 045F 550 |
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Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada |
| abstract |
• Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion younger (2717Ma) and unrelated to Wabassi Intrusive Complex. |
| abstractGer |
• Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion younger (2717Ma) and unrelated to Wabassi Intrusive Complex. |
| abstract_unstemmed |
• Max, Wabassi Main, and Wabassi South intrusions form the Wabassi Intrusive Complex. • Wabassi Intrusive Complex formed between 2728 and 2727Ma. • All parental magmas are basaltic (up to ∼12% MgO). • Max intrusion may be the most prospective area for Ni–Cu–(PGE) exploration. • Oxtoby Lake intrusion younger (2717Ma) and unrelated to Wabassi Intrusive Complex. |
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GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 |
| title_short |
Age constraints and geochemical evolution of the Neoarchean mafic–ultramafic Wabassi Intrusive Complex in the Miminiska–Fort Hope greenstone belt, Superior Province, Canada |
| url |
https://doi.org/10.1016/j.precamres.2016.09.018 |
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| author2 |
Houlé, M.G. Lesher, C.M. McNicoll, V. Vaillancourt, C. Kamber, B.S. |
| author2Str |
Houlé, M.G. Lesher, C.M. McNicoll, V. Vaillancourt, C. Kamber, B.S. |
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| doi_str |
10.1016/j.precamres.2016.09.018 |
| up_date |
2024-07-06T17:10:47.090Z |
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