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Cited by 591

The DOI matches its Crossref record; 70 of the 70 references it cites were found in a registry or an index.

A History of Continents in the past Three Billion Years

Rogers, John J. W.·1996·The Journal of Geology

Abstract

The end-Paleozoic Pangea appears to have contained three continents that had grown in the Precambrian and remained intact until Mesozoic rifting: Ur, formed at ~3 Ga and accreted to most of East Antarctica in the middle Proterozoic to form East Gondwana; Arctica, an approximately 2.5-2 Ga continent that contained Archean terranes of the Canadian and Siberian shields and Greenland; and Atlantica, formed at ~2 Ga of cratons of ~2 Ga age that now occur in West Africa and eastern South America. Arctica grew at ~1.5 Ga by accretion of most of East Antarctica plus Baltica to form the continent of Nena. Collision of Nena, Ur, and Atlantica, plus minor plates, formed the supercontinent of Rodina at ~1 Ga. Rifting of Rodinia between 1 and 0.5 Ga formed three continents: East Gondwana; Atlantica (which became the nucleus for West Gondwana); and Laurasia (which contained North America, Greenland, Baltica, and Siberia). Gondwana formed at ~0.5 Ga by amalgamation of its eastern and western parts. Various plates accreted to Laurasia during the Paleozoic, and collision of Gondwana with Laurasia created Pangea at ~0.3 Ga.

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Metadata

Authors
Rogers, J. J. W.
Venue
The Journal of Geology
Published
1996-01
Volume
104
Issue
1
Pages
91-107
ISSN
  • 0022-1376 (ISSN-L)
  • 1537-5269
OpenAlex
W2028837424
Cited by
591
References
70
FWCI
13.04
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: A History of Continents in the past Three Billion Years. https://app.cochat.ai/papers/10.1086/629803
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Rogers, J. J. W. (1996). A History of Continents in the past Three Billion Years. The Journal of Geology. https://doi.org/10.1086/629803

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