The Ediacaran Apparent Polar Wander Path of the Río de la Plata craton revisited: Paleogeographic implications.
- 1Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA), University of Buenos Aires, Buenos Aires, Argentina
- 2CONICET, Argentina
- 3Instituto de Hidrología de Llanuras “Dr. E. J. Usunoff”, CONICET, Argentina
- 4Centro de Investigaciones Geológicas (UNLP-CONICET), Facultad de Ciencias Naturales y Museo, La Plata, Argentina
- 5Departamento de Geofísica, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, São Paulo, Brazil
The Ediacaran apparent polar wander path for the Rio de la Plata Craton was analyzed and a new alternative path is presented. This revised path was constructed considering an opposite polarity for poles older than ca. 590 Ma. This path is more consistent with that recently proposed for West Africa, whose large oscillations were attributed to two events of inertial interchange true polar wander (IITPW). A compilation and selection of Ediacaran paleomagnetic data from the main cratons were analyzed leading to a set of global paleogeographic reconstructions throughout the Ediacaran. This model assumes that a “Clymene Ocean” existed between Central Gondwana and West Africa – Amazonia along this period. All cratons with reliable paleomagnetic information, share similar motions during two time-intervals. The first one (615-590 Ma) can be described by rotation around an Euler pole located in the equator, while the second one (575-565 Ma) by another around an Euler pole on the tropics. Whether these apparent large and fast displacements can be assigned to IITPW events is discussed along with the consistency of considering a large Clymene Ocean during this time.
How to cite: Cukjati, A., Franceschinis, P., Arrouy, M. J., Gómez-Peral, L., Poiré, D., Trindade, R., and Rapalini, A.: The Ediacaran Apparent Polar Wander Path of the Río de la Plata craton revisited: Paleogeographic implications., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-463, https://doi.org/10.5194/egusphere-egu24-463, 2024.