Geochemistry of Komatiites in the Abitibi Greenstone Belt and Implications for Their Mineralization Potential
- Organization:
- Canadian Institute of Mining, Metallurgy and Petroleum
- Pages:
- 30
- File Size:
- 4621 KB
- Publication Date:
- May 1, 2003
Abstract
Abitibi Greenstone Belt ? ~2.745 to 2.680 Ga (U-Pb zircon ages) ? Several lithologically-distinct and structurally repeated(?) assemblages ? Represents: ? Allochthonous terranes? ? Single autochthonous terrane? ? Combination of the above Volcanology of Komatiites in the Abitibi greenstone belt ? Tisdale and Kidd-Munro assemblages have channelized flows ? Pacaud and Stoughton-Roquemaure assemblages DO NOT have channelized flows ? Only Tisdale and Kidd-Munro assemblages are mineralized
Citation
APA: (2003) Geochemistry of Komatiites in the Abitibi Greenstone Belt and Implications for Their Mineralization Potential
MLA: Geochemistry of Komatiites in the Abitibi Greenstone Belt and Implications for Their Mineralization Potential. Canadian Institute of Mining, Metallurgy and Petroleum, 2003.