Did the Breakout of Laurentia Turn Gondwanaland Inside-Out?
Comparative geology suggests that the continents adjacent to northern, western, southern, and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern Africa, and Amazonia-Baltica, respectively. Late Proterozoic fragmentation of the supercontinent centered on Laurentia...
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American Association for the Advancement of Science (AAAS)
1991
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Online Access: | http://dx.doi.org/10.1126/science.252.5011.1409 https://www.science.org/doi/pdf/10.1126/science.252.5011.1409 |
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craaas:10.1126/science.252.5011.1409 2024-09-09T19:06:15+00:00 Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? Hoffman, Paul F. 1991 http://dx.doi.org/10.1126/science.252.5011.1409 https://www.science.org/doi/pdf/10.1126/science.252.5011.1409 en eng American Association for the Advancement of Science (AAAS) Science volume 252, issue 5011, page 1409-1412 ISSN 0036-8075 1095-9203 journal-article 1991 craaas https://doi.org/10.1126/science.252.5011.1409 2024-08-29T04:00:39Z Comparative geology suggests that the continents adjacent to northern, western, southern, and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern Africa, and Amazonia-Baltica, respectively. Late Proterozoic fragmentation of the supercontinent centered on Laurentia would then have been followed by rapid fan-like collapse of the (present) southern continents and eventual consolidation of East and West Gondwanaland. In this scenario, a pole of rotation near the Weddell Sea would explain the observed dominance of wrench tectonics in (present) east-west trending Pan-African mobile belts and subduction-accretion tectonics in north-south trending belts. In the process of fragmentation, rifts originating in the interior of the Late Proterozoic supercontinent became the external margins of Paleozoic Gondwanaland; exterior margins of the Late Proterozoic supercontinent became landlocked within the interior of Gondwanaland. Article in Journal/Newspaper Antarc* Antarctica Weddell Sea Siberia AAAS Resource Center (American Association for the Advancement of Science) Weddell Weddell Sea Science 252 5011 1409 1412 |
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AAAS Resource Center (American Association for the Advancement of Science) |
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English |
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Comparative geology suggests that the continents adjacent to northern, western, southern, and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern Africa, and Amazonia-Baltica, respectively. Late Proterozoic fragmentation of the supercontinent centered on Laurentia would then have been followed by rapid fan-like collapse of the (present) southern continents and eventual consolidation of East and West Gondwanaland. In this scenario, a pole of rotation near the Weddell Sea would explain the observed dominance of wrench tectonics in (present) east-west trending Pan-African mobile belts and subduction-accretion tectonics in north-south trending belts. In the process of fragmentation, rifts originating in the interior of the Late Proterozoic supercontinent became the external margins of Paleozoic Gondwanaland; exterior margins of the Late Proterozoic supercontinent became landlocked within the interior of Gondwanaland. |
format |
Article in Journal/Newspaper |
author |
Hoffman, Paul F. |
spellingShingle |
Hoffman, Paul F. Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
author_facet |
Hoffman, Paul F. |
author_sort |
Hoffman, Paul F. |
title |
Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
title_short |
Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
title_full |
Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
title_fullStr |
Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
title_full_unstemmed |
Did the Breakout of Laurentia Turn Gondwanaland Inside-Out? |
title_sort |
did the breakout of laurentia turn gondwanaland inside-out? |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1991 |
url |
http://dx.doi.org/10.1126/science.252.5011.1409 https://www.science.org/doi/pdf/10.1126/science.252.5011.1409 |
geographic |
Weddell Weddell Sea |
geographic_facet |
Weddell Weddell Sea |
genre |
Antarc* Antarctica Weddell Sea Siberia |
genre_facet |
Antarc* Antarctica Weddell Sea Siberia |
op_source |
Science volume 252, issue 5011, page 1409-1412 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.252.5011.1409 |
container_title |
Science |
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252 |
container_issue |
5011 |
container_start_page |
1409 |
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1412 |
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1809820299066081280 |