Rodinia

Rodinia (ex Russico родить 'parere'Li, Z. X.; Bogdanova, S. V.; Collins, A. S.; Davidson, A.; B. De Waele, R. E. Ernst, I. C. W. Fitzsimons, R. A. Fuck, D. P. Gladkochub, J. Jacobs, K. E. Karlstrom, S. Lul, L.M. Natapov, V. Pease, S. A. Pisarevsky, K. Thrane and V. Vernikovsky (2008). "Assembly, configuration, and break-up history of Rodinia: A synthesis". Precambrian Research 160: 179–210) in geologia est supercontinens, continens qui plurimas vel omnes terras emersas continuit. Secundum refectiones laminarum tectonicarum, Rodinia tempore abhinc annorum inter 1.1 billiones et 750 milliones existitit, aera Neoproterozoica. Natus est circa 1.0 Ga per accretionem et concursum fragmentorum a dissolutione vetustioris supercontinentis, Columbiae, effecta. Rodinia in animo populari est unus ex duobus magnis historiae Telluris supercontinentibus, quorum alius est Pangaea.

 Circulus supercontinentium
 Columbia (supercontinens)

 Notae 

 Bibliographia 


















 Nexus externi 

 "Dance of the Giant Continents: Washington's Earliest History"
 IGCP Special Project 440: mapping Proterozoic supercontinents, including Rodinia
 PALEOMAP Project: Plate Tectonic Animations (java)
  by Dean Praetorius

Categoria:Supercontinentes
Categoria:Continentes praehistoricae