Mortensen, J. K. (1993) U–Pb geochronology of the eastern Abitibi Subprovince. Part 2: Noranda – Kirkland Lake area. Canadian Journal of Earth Sciences, 30 (1) 29-41 doi:10.1139/e93-003
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | U–Pb geochronology of the eastern Abitibi Subprovince. Part 2: Noranda – Kirkland Lake area | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | Mortensen, J. K. | Author | |
| Year | 1993 (January 1) | Volume | 30 |
| Issue | 1 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e93-003Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 481904 | Long-form Identifier | mindat:1:5:481904:6 |
| GUID | 0 | ||
| Full Reference | Mortensen, J. K. (1993) U–Pb geochronology of the eastern Abitibi Subprovince. Part 2: Noranda – Kirkland Lake area. Canadian Journal of Earth Sciences, 30 (1) 29-41 doi:10.1139/e93-003 | ||
| Plain Text | Mortensen, J. K. (1993) U–Pb geochronology of the eastern Abitibi Subprovince. Part 2: Noranda – Kirkland Lake area. Canadian Journal of Earth Sciences, 30 (1) 29-41 doi:10.1139/e93-003 | ||
| In | (1993, January) Canadian Journal of Earth Sciences Vol. 30 (1) Canadian Science Publishing | ||
| Abstract/Notes | U–Pb zircon ages for 15 volcanic and plutonic units in the Noranda and Kirkland Lake areas help constrain the history of volcanism, plutonism, sedimentation, and deformation in the south-central part of the Abitibi belt. Volcanism occurred over an interval of at least 50 Ma, beginning with the deposition of the volcanic and volcaniclastic units within the Pacaud Structural Complex at 2747 Ma. Following a period of apparent quiescence, magmatism resumed at 2730–2725 Ma with the eruption of volcanic rocks in the Normétal and Lac Abitibi area. From 2715 until about 2698 Ma, volcanism occurred sporadically throughout much of the area, culminating in the eruption of the Blake River Group from 2703 to 2698 Ma. Several large intrusive bodies yield ages that indicate that they are plutonic equivalents of the Blake River Group. Plutons that are considered to have been emplaced during the Kenoran orogeny give ages that are only slightly younger than the youngest volcanic units of the Blake River Group, emphasizing the very rapid onset of Kenoran deformation following the cessation of volcanic activity.The Cléricy syenite, dated at 2682 ± 3 Ma, postdates the main period of Kenoran deformation in this area and intrudes sedimentary rocks of the Kewagama Group which contain detrital zircons as young as 2687 Ma. These data suggest that the Kewagama Group is the same age as late sedimentary sequences such as the Timiskaming Group and may have been deposited in a similar tectonic setting. | ||
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