Neoproterozoic tectonic geography was dominated by the formation of the supercontinent
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …

Abstract The Early Proterozoic evolution of the São Francisco craton (SFC) occurred
between 1.8–2.5 Ga and includes the Transamazonian cycle (1.9–2.2 Ga), one of the main …

This paper presents a brief synthesis of the current state of knowledge on the formation and
break-up of the early-Neoproterozoic supercontinent Rodinia, and the subsequent assembly …

During the Neoproterozoic, a supercontinent commonly referred to as Rodinia, supposedly
formed at ca. 1100 Ma and broke apart at around 800–700 Ma. However, continental fits (eg …

The Borborema Province of NE Brasil comprises the central part of a wide Pan-African-
Brasiliano orogenetic belt that formed as a consequence of late Neoproterozoic …

Palaeomagnetic apparent polar wander (APW) paths from the world's cratons at 1300–700
Ma can constrain the palaeogeographic possibilities for a long-lived and all-inclusive …

The identification of large igneous provinces (LIPs) and associated mantle plumes has been
confined for the most part to the Mesozoic and Cenozoic record. With few exceptions, pre …

Amongst existing palaeogeographic models of the Rodinia supercontinent, or portions
thereof, arguments have focused upon geological relations or palaeomagnetic results, but …

Palaeomagnetic data are used to study the configurations of continents during the
Proterozoic. Applying stringent reliability criteria, the positions of the continents at 12 times in …

Well-dated paleomagnetic poles for the interval 1100–800 Ma have been compiled for the
Laurentia, Baltica, São Francisco, Congo and Kalahari cratons in order to construct apparent …