Pampia

Today, Pampia is a topic of great relevance and interest to a wide range of people and communities. Whether due to its impact on society, its cultural relevance or its importance in the academic field, Pampia has captured the attention of many, generating debates, reflections and research around this topic. From different perspectives and approaches, Pampia has aroused great interest due to its influence on various aspects of daily life. In this article, we will explore different facets of Pampia, analyzing its importance, implications and possible future developments.

Pampia was an ancient microcontinent or terrane that collided with Río de la Plata Craton and Río Apas Craton during the Pampean orogeny of late Proterozoic and early Cambrian. It was one of the first terranes to be amalgamated to the old cratons of the east, and was followed by the suturing of Cuyania and Chilenia terranes into the young South American Plate.

References

  1. ^ Casquet, C; Rapela, C.W; Pankhurst, R.J; Baldo, E.G; Galindo, C; Fanning, C.M; Dahlquist, J.A; Saavedra, J (2012). "A history of Proterozoic terranes in southern South America: From Rodinia to Gondwana". Geoscience Frontiers. 3 (2): 137–45. Bibcode:2012GeoFr...3..137C. doi:10.1016/j.gsf.2011.11.004. hdl:1885/52238.
  2. ^ Gaucher, Claudio; Bossi, Jorge; Blanco, Gonzalo (2009). "Palaeogeography". Neoproterozoic-Cambrian Tectonics, Global Change and Evolution: A Focus on South Western Gondwana. Developments in Precambrian Geology. Vol. 16. pp. 131–41. doi:10.1016/S0166-2635(09)01609-0. ISBN 978-0-444-53249-7.

Sources