Deeply concealed half-graben at the SW margin of the East European Craton (SE Poland) — Evidence for Neoproterozoic rifting prior to the break-up of Rodinia

Deeply concealed half-graben at the SW margin of the East European Craton (SE Poland) — Evidence for Neoproterozoic rifting prior to the break-up of Rodinia

Baltica was one of continents formed as a result of Rodinia break-up 850–550 Ma. It was separated from Amazonia(?) by the Tornquist Ocean, the opening of which was preceded by Neoproterozoic extension in a network of continental rifts. Some of these rifts were subsequently aborted whereas the Tornqu...

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Bibliographic Details
Main Authors: P. Krzywiec, P. Poprawa, M. Mikołajczak, S. Mazur, M. Malinowski
Format: Article
Language:English
Published: SpringerOpen 2018-01-01
Series:Journal of Palaeogeography
Subjects:
Rodinia
Baltica
Tornquist rift
Orsha-Volyn Aulacogen
Tornquist Ocean
Neoproterozoic
Seismic data
Gravity data
Online Access:http://www.sciencedirect.com/science/article/pii/S2095383617300913

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http://www.sciencedirect.com/science/article/pii/S2095383617300913

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