| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4724131 | Precambrian Research | 2008 | 10 Pages |
In an attempt to improve our understanding of the Paleoproterozoic geodynamic evolution, a paleomagnetic study was performed on 10 sites of acid volcanic rocks of the Colider Suite, southwestern Amazonian Craton. These rocks have a well-dated zircon U–Pb mean age of 1789 ± 7 Ma. Alternating field and thermal demagnetization revealed northern (southern) directions with moderate to high upward (downward) inclinations. Rock magnetism experiments and magnetic mineralogy show that this characteristic magnetization is carried by Ti-poor magnetite or by hematite that replaces magnetite by late-magmatic deuteric alteration. Both magnetite and hematite carry the same characteristic component. The mean direction (Dm = 183.0°, Im = 53.5°, N = 10, α95 = 9.8°, K = 25.2) yielded a paleomagnetic pole located at 298.8°E, 63.3°S (α95 = 10.2°, K = 23.6), which is classified with a quality factor Q = 5. Paleogeographic reconstructions using this pole and other reliable Paleoproterozoic poles suggest that Laurentia, Baltica, North China Craton and Amazonian Craton were located in laterally contiguous positions forming a large continental mass at 1790 Ma ago. This is reinforced by geological evidence which support the existence of the supercontinent Columbia in Paleoproterozoic times.
