Volume 1 Quaternary Chapter 6 Neogene https://doi.org/10.32685/pub.esp.35.2019.06 The Putumayo Orogen of Amazonia: A Synthesis Published online 24 November 2020 Mauricio IBAÑEZ–MEJIA1* Paleogene Abstract Meso– and Neoproterozoic paleogeographic reconstructions indicate that Amazonia played an important role in the assembly of Rodinia, and that its incorpora- tion into this supercontinent led to continent–continent collision(s) with the Grenville 1
[email protected] Orogen of Laurentia and the Sveconorwegian Orogen of Baltica. The Sunsás–Agua- Department of Geosciences Cretaceous peí belt of SW Amazonia has traditionally been regarded as the geological evidence University of Arizona Tucson, Arizona, 85721, USA* of such interactions, although it is becoming increasing clear that the metamorphic Corresponding author and tectonic history of this margin does not match the grade and timing that would be expected from interactions with the (near)–Adirondian margin of the Grenville, or Jurassic with the Sveconorwegian margin of Fennoscandia. Massifs of amphibolite– to granu- lite–facies basement of late Proterozoic age have been known to exist in the northern Andes for many decades, but an autochthonous late Meso– to early Neoproterozoic orogenic belt in the western Guiana Shield that is un–remobilized by Andean tectonics, remained unknown. The recent discovery of such a belt, hidden under the Putumayo Triassic Foreland Basin, allowed, for the first time, to directly link the basement inliers of the Colombian Andes with the western Guiana Shield. Furthermore, the improved geo- chronologic database of some cordilleran inliers and Putumayo Basin basement, using high–spatial–resolution U–Pb methods, has permitted a more complete reconstruction Permian of their evolution.