Paleomagnetism of the Ediacaran Avellaneda Formation (Argentina), part I: Paleogeography of the Río de la Plata craton at the dawn of Gondwana

A paleomagnetic and rock magnetic study was carried out in the Ediacaran Avellaneda (~570 Ma) and Cerro
Negro (~555 Ma) Formations belonging to the La Providencia Group, in the upper part of the Neoproterozoic
sedimentary cover of the Tandilia region, in the Río de la Plata craton. The Avellaneda Formation was studied at
outcrop level and in three drill cores, yielding a mean characteristic remanence direction of Dec: 21.4◦, Inc:
67.1◦, α95: 4.2◦, k: 23.9, N: 51 and a paleomagnetic pole at 1.0◦ S, 313.4◦ E, A95: 5.9◦. The Cerro Negro Formation
yielded a mean characteristic direction of Dec: 22.0◦, Inc: 68.5◦, α95: 10.3◦, k: 20.8, N: 11 obtained from a single
drill core, from which a paleomagnetic pole at 3.6◦ S, 307.8◦E, A95: 16.6◦ was computed. Rock magnetic data
indicates that magnetic remanence is mainly associated with magnetite and hematite. The paleomagnetic information
presented here results in a change in the previously accepted Late Ediacaran apparent polar wander
path of the Río de la Plata Craton. The newly obtained poles indicate that Río de la Plata Craton experienced a
rapid drift from a low latitudes location (ca. 19◦ S) at ca. 600 Ma to moderately higher latitudes (between 50◦
and 42◦S) from around 580 to 550 Ma.